This work was funded by the Swiss National Science Foundation (grant n&#176; 200021-140230) and by the Swiss Federal Office of Public Health (PF and PS). We thank the Swiss Federal Office of Public Health for providing financial support for the open-access publication of this paper.

1. Plutonium Tracer Preparation
<ol>
	<li>Pu(IV) tracer preparation
	<ol>
		<li>From the Pu stock solution transfer an appropriate aliquot containing the desired amount of Pu for the experiment into a 25 ml glass beaker. Work with 10 Bq of 239Pu at a time.</li>
		<li>Add 1 ml concentrated HNO3, 0.6 ml 1 M NaHSO4, 0.4 ml concentrated H2SO4. Evaporate to dryness on a hot plate. Heat slowly at 200 &#176;C at the beginning to avoid acid projection.</li>
		<li>Once no liquid is left in the beaker, anneal the residue at 400 &#176;C &#8211; 500 &#176;C until no white fumes emanate. The residue is white when cooled and soluble in the buffer chosen for the experiment. 
		Note: Pu(IV) source prepared in this way can be stored dry up to several months12.</li>
	</ol>
	</li>
	<li>&#8203;Pu(V) tracer preparation13&#160;
	<ol>
		<li>Pu oxidation
		<ol>
			<li>Transfer an aliquot from the Pu stock solution into a plastic 20 ml liquid-scintillation vial with a leakproof cap. Work with 10 Bq of 239Pu at a time. Add 0.01 ml of 0.01 M KMnO4 and leave the mixture in the dark for at least 6 hr.</li>
		</ol>
		</li>
		<li>Pu(VI) extraction
		<ol>
			<li>Prior to extraction prepare a solution of 0.5 M thenoyltrifluoroacetone (TTA) in cyclohexane and protect it from light exposure. Always prepare this solution immediately prior to each experiment.</li>
			<li>Add to the oxidized Pu solution 2 ml of 0.1 M CH3COONa at pH 4.7 and 2 ml of 0.5 M thenoyltrifluoroacetone (TTA) in cyclohexane. Wrap the bottle with aluminum foil to keep the reaction mixture in the dark, shake for 10 min. Separate the organic phase containing Pu(VI) with a pipette and transfer to a clean glass vial.</li>
		</ol>
		</li>
		<li>Pu(VI) to Pu(V) photoreduction
		<ol>
			<li>Leave the glass vial containing Pu(VI)-TTA complex in cyclohexane at room light for 2 hr.</li>
		</ol>
		</li>
		<li>Pu(V) extraction
		<ol>
			<li>Add to the light-exposed solution 1 ml of 0.1 M CH3COONa at pH 4.7 and shake for 5 min. Remove aqueous phase, containing Pu(V). Determine the concentration of this source by liquid scintillation counting taking a 100 &#181;l aliquot. 
			Note: Prepare Pu(V) solutions immediately prior to each experiment since the long-term stability of Pu in +V oxidation state is being questioned.</li>
		</ol>
		</li>
	</ol>
	</li>
</ol>
2. Preparation of the Solutions Used in the Experiments
<ol>
	<li>Prepare buffered solutions
	<ol>
		<li>Make 10 mM solution of MOPS (3-(N-morpholino)propanesulfonic acid) buffer. Take 200 ml of this solution and adjust to the desired pH by drop wise addition of 0.1 M HCl (pH 6.5 for use with Pu(IV) and pH 5.5 for use with Pu(V)).</li>
	</ol>
	</li>
	<li>Prepare solutions for experiments with Pu(IV)
	<ol>
		<li>Solution A
		<ol>
			<li>Dissolve Pu(IV) prepared at the step 1.1 in several milliliters of 10 mM MOPS buffered solution at pH 6.5. Thoroughly wash the beaker with the same solution.</li>
			<li>Bring the volume to 72 ml with 10 mM MOPS buffered solution at pH 6.5. Check the pH and re-adjust to 6.5 with 0.1 M NaOH. Transfer 72 ml of this solution into a clean beaker &#8212; this is the (A) solution to be introduced into compartment A of the diffusion cell.</li>
		</ol>
		</li>
		<li>Solution B
		<ol>
			<li>Take 72 ml of 10 mM MOPS buffered solution at pH 6.5; add 0.75 ml of 1 M Na2SO4. Check the pH, re-adjust to 6.5 if necessary. Transfer 72 ml of this solution into a clean beaker &#8212; this is the &#171;&#160;B&#160;&#187; solution to be introduced into &#171;&#160;B&#160;&#187; compartment of the diffusion cell.</li>
		</ol>
		</li>
		<li>Prepare solutions with NOM
		<ol>
			<li>Weigh 1.4 mg of freeze-dried fulvic or humic acid to a obtain concentration of 20 ppm and dissolve it in the &#171;&#160;A&#160;&#187; solution containing Pu(IV). Prepare this solution 24 hr prior to experiment and to allow for equilibration.</li>
		</ol>
		</li>
	</ol>
	</li>
	<li>Prepare solutions for experiments with Pu(V)
	<ol>
		<li>Solution&#160;A&#160;
		<ol>
			<li>Dissolve Pu(V) obtained at the step 1.2.4 in 72 ml of 10 mM MOPS buffered solution at pH 5.5; add 0.75 ml of 1 M NaNO3. Check the pH and adjust to 5.5 if necessary. Transfer 72 ml of this solution into a clean beaker. Prepare the solution with Pu(V) immediately prior to experiment.</li>
		</ol>
		</li>
		<li>Solution&#160;B
		<ol>
			<li>Take 72 ml of 10 mM MOPS buffered solution at pH 5.5; add 0.75 ml of 1 M NaNO3. Check the pH and adjust to 5.5 if necessary. Transfer 72 ml of this solution into a clean beaker.</li>
		</ol>
		</li>
		<li>Prepare solutions with NOM
		<ol>
			<li>Weigh 1.4 mg of freeze-dried fulvic or humic acid to obtain a concentration of 20 ppm and dissolve in the&#160;A solution containing Pu(V). Leave the solution for 24 hr to reach the steady state between Pu(IV) and Pu(V) species. Prior to diffusion experiment perform a liquid phase extraction to determine the fraction of Pu(V) as described in the Section 3.4.2.</li>
		</ol>
		</li>
	</ol>
	</li>
</ol>
3. Laboratory Diffusion Experiments
<ol>
	<li>Prepare PAM gel
	<ol>
		<li>Wet a plastic tray with several milliliters of electrolyte (e.g., 10 mM NaNO3), place the PAM gel strip in and expand uniformly over the surface. Place cautiously a sharp punch of 2.7 cm in diameter on the gel surface. Avoid sliding the punch over the gel surface.</li>
		<li>Use local focused lighting if necessary, it may help to visualize the transparent PAM gel. Press the punch firmly against gel surface and release once it is cut.</li>
	</ol>
	</li>
	<li>Assembly of the diffusion cell
	<ol>
		<li>Position the PAM gel disc with tweezers into the groove over the diffusion window in a smooth-faced manner. Turn the screw such that the two compartments of the diffusion cell hold together, interconnected via the PAM gel disc.</li>
		<li>Mark A and B diffusion cell&#39;s compartments. Assemble the diffusion cell with the gel disc immediately prior to each experiment; do not allow the gel to dry.</li>
	</ol>
	</li>
	<li>Launching a diffusion experiment
	<ol>
		<li>Slowly pour the A and B solutions into the corresponding compartments. Make sure that both solutions are poured at the same speed in order to provide equal volume in each compartment at any time, otherwise the diffusive gel can be damaged.</li>
		<li>Launch the timer once the solutions are in the cell. Place the miniature electric mixers over the diffusion cell. At this time the diffusion experiment is considered started.</li>
	</ol>
	</li>
	<li>Taking samples throughout diffusion experiment
	<ol>
		<li>Take samples of equal volume within regular time intervals from the A and B compartments simultaneously in order to keep volumes constant throughout the experiment.
		<ol>
			<li>Take a 1.00 ml sample simultaneously in each compartment immediately at the beginning of the experiment to determine the initial Pu concentration in the A compartment.</li>
			<li>Use a sampling time interval of 10 min in experiments without addition of NOM and 20 min to several h in experiments with humic acid. 2.00 ml aliquots are sufficient to provide good sensitivity for alpha-spectrometric measurements.</li>
		</ol>
		</li>
		<li>Liquid phase extraction of Pu(IV) and Pu(V)
		<ol>
			<li>At the end of the diffusion experiment take separately 4 ml samples from the A and the B compartments into plastic test-tubes with leakproof caps. Acidify samples with 1 ml 2 M HCl.</li>
			<li>Add 5 ml of 0.5 M bis-(2-ethyl hexyl) phosphoric acid (HDEHP) solution in cyclohexane and agitate test-tubes vigorously for 5 min. Leave samples to allow for phase separation. Remove the water phase containing Pu(V).</li>
		</ol>
		</li>
		<li>Back-extraction of Pu(IV)
		<ol>
			<li>Back-extract Pu(IV) from the remaining organic phase with 5 ml of 5% (NH4)2C2O4.</li>
		</ol>
		</li>
	</ol>
	</li>
</ol>
4. Sample Treatment
<ol>
	<li>Spike samples with an internal standard
	<ol>
		<li>Spike samples to be analyzed with a yield tracer. Use a spike of 1.00 ml of 242Pu tracer of 25 mBq ml-1 activity concentration for alpha-spectrometric measurements.</li>
	</ol>
	</li>
	<li>Oxidize samples&#8217; matrix
	<ol>
		<li>Evaporate samples to dryness on a hot plate with 2.00 ml of concentrated HNO3.</li>
	</ol>
	</li>
</ol>
5. Radiochemical Separation of Pu
<ol>
	<li>Adjust Pu oxidation state
	<ol>
		<li>Dissolve dry samples from point 4.2.1 in 5 ml 8 M HNO3, add 20 mg NaNO2, heat samples at 70 &#176;C during 10 min. This step allows adjusting the oxidation state of Pu to +IV.</li>
	</ol>
	</li>
	<li>Solid phase extraction of Pu
	<ol>
		<li>Wet a quaternary amine-based anion exchange resin column (such as TEVA) with 1.5 ml 8 M HNO3. Use micro-columns made of 1 ml pipette tip with 100 mg of the resin conditioned with 1.5 ml 8 M HNO3.</li>
		<li>Pass the solution of point 5.1.1 through the resin column with flow rate of about 1 ml min-1. Rinse the sample beaker with 2 ml 8 M HNO3 three times and transfer washouts to resin columns.</li>
	</ol>
	</li>
	<li>Elute Pu
	<ol>
		<li>Wash columns with 3 ml 9 M HCl. Elute Pu with 3 ml solution 9 M HCl/0.1 M HI. Evaporate eluates on the hot plate. Treat with 2 ml concentrated HNO3, evaporate to dryness. Repeat if necessary until the brown iodine color disappears.</li>
		<li>Determine Pu concentration in the samples by any available method. 
		Note. For the concentrations range of 239Pu used in this protocol alpha-spectrometry provides a good sensitivity. Prepare sources for alpha-spectrometric counting by electroplating on stainless steel discs14. Count sources on PIPS detector (450 mm2) in a spectrometer.</li>
	</ol>
	</li>
</ol>
6. Analysis of the Data
<ol>
	<li>Plot diffused Pu versus time
	<ol>
		<li>Plot the activity of Pu (mBq) accumulated in the B compartment versus time (min). Correct for volume of the sample taken out during the diffusion experiment: activity of accumulated Pu (mBq) at time t is equal to the concentration (mBq ml-1) determined in the sample multiplied by the volume of the solution (ml) in the compartment B at the moment of sampling (see example of the spreadsheet &#8212; Figure 2).</li>
		<li>To plot on the same graph data from several experiments with different Pu concentrations, use concentrations normalized to the initial Pu concentration of compartment A.</li>
	</ol>
	</li>
	<li>Calculate diffusion coefficient
	<ol>
		<li>Calculate diffusion coefficient D (cm2 sec-1) of Pu species for each experiment10. Use equation (1): 
		<img alt="Equation 1" src="/files/ftp_upload/53188/53188eq1.jpg" />&#160;&#160;&#160;&#160; (1) 
		where &#916;g is the diffusion gel thickness (cm), C the initial Pu concentration (mBq ml-1), S the diffusion area (cm2), and A the activity (mBq) of Pu species diffused in compartment B at the time t (sec). &#916;A/&#916;t is the slope of the linear plot of Pu diffused into the B compartment versus time.</li>
	</ol>
	</li>
</ol>
7. Bioavailability Studies of Pu in Natural Freshwaters
<ol>
	<li>Prepare DGT samplers
	<ol>
		<li>Wet a plastic tray with several milliliters of electrolyte (e.g., 10 mM NaNO3), place the bottom plate (see Figure 3) of the DGT sampler. Use local lighting if necessary, it may help to visualize transparent gels.</li>
		<li>Position a 6 cm &#215; 22 cm Chelex resin gel strip and expand uniformly over the plate&#8217;s surface. Place on the top of the resin gel layer a 6 cm &#215; 22 cm PAM diffusive gel strip and expand uniformly over the surface. Make sure that gels are not sliding and are positioned in a smooth-faced manner.</li>
		<li>Cover the diffusive gel layer with a 6 cm &#215; 22 cm piece of a filter membrane. Place the cover frame of the DGT sampler (see Figure 3) over the filter membrane and close the assembly slightly pressing the frame on the edges.</li>
		<li>Cut the extending gel parts off with a sharp lancet, open and realign gel layers if necessary until a smooth plate surface is obtained. Fix the assembly with screws.</li>
		<li>Wet the DGT samplers with several milliliters of electrolyte (e.g., 10 mM NaNO3). Store wet in a sealed plastic bag up to several weeks at 4-5 &#176;C.</li>
	</ol>
	</li>
	<li>Deployment of DGTs in a natural body of water
	<ol>
		<li>Take the DGT sampler out of the plastic bag. Fix DGT samplers in the holder as shown on the Figure 4.</li>
		<li>Deploy DGTs in the body of water either suspending them on a strong rope or installing on a stable vertical support in a way to provide a constant tangential water flow along the surface of the DGT. Deploy DGT devices in the freshwaters for two to three weeks in order to accumulate the Pu at a concentration sufficient for measurements.</li>
	</ol>
	</li>
	<li>Treatment of retrieved DGTs
	<ol>
		<li>Retrieve DGTs from the water. Unscrew the assembly, take out filter membrane and discard. Take out the upper gel layer (PAM diffusive gel) and discard.</li>
		<li>Transfer the resin gel into a glass beaker containing 20 ml 8 M HNO3 and spike samples to be analyzed with a yield tracer. Use a spike of 1.00 ml of 242Pu tracer of 0.25 mBq ml-1 (1.7 pg ml-1) activity concentration for AMS measurements. After having well agitated, leave samples O/N for Pu elution.</li>
	</ol>
	</li>
	<li>Condition DGT eluates
	<ol>
		<li>Filter the solutions from the resin gel samples; rinse the remaining resin gels with 5 ml 8 M HNO3 and combine washouts with samples. Add 20 mg NaNO2 to each sample, heat the solutions at 70 &#176;C during 10 min. This step allows adjusting the oxidation state of Pu to +IV.</li>
	</ol>
	</li>
	<li>Solid phase extraction of Pu
	<ol>
		<li>Wet a quaternary amine-based anion exchange resin cartridge with 10 ml 8 M HNO3. Pass the solutions of point 7.4.1 through the exchange resin cartridge with flow rate of about 1 ml min-1. Rinse the sample beaker with 5 ml 8 M HNO3 three times and transfer the washouts to exchange resin cartridge.</li>
	</ol>
	</li>
	<li>Elute Pu
	<ol>
		<li>Wash cartridges with 10 ml 9 M HCL. Elute Pu with 15 ml solution 9 M HCl/0.1 M HI. Evaporate eluate on a hot plate. Treat with 2 ml concentrated HNO3, evaporate to dryness. Repeat if necessary until the brown iodine color has completely disappeared.</li>
		<li>Repeat radiochemical separation of Pu one to two more times if higher purification is required &#8212; depending on the performance of Pu detecting system. Perform the second and the third separations on micro-columns made of 1 ml pipette tip with 100 mg of exchange resin conditioned with 1.5 ml 8 M HNO3.</li>
		<li>Determine Pu concentration in the samples. Use the mass-spectrometry techniques to measure 239Pu because of the very low level of plutonium in the pristine environment. 
		Note: In this work, use the AMS facility tuned for analysis of actinides at the Laboratory of Ion Beam Physics at the Swiss Federal Institute of Technology in Zurich.</li>
	</ol>
	</li>
</ol>
8. Analysis of the Data
<ol>
	<li>Calculate the concentration (CDGT in &#181;Bq ml-1) of bioavailable (labile) Pu species in the bulk water from the amount of Pu accumulated by DGT during the deployment period. Use equation (2): 
	<img alt="Equation 2" src="/files/ftp_upload/53188/53188eq2.jpg" />&#160;&#160;&#160;&#160; (2) 
	where A is the activity (&#181;Bq) of Pu accumulated in the binding phase, &#916;g the diffusion layer (gel + filter membrane) thickness (cm), D the diffusion coefficient of Pu in the PAM gel (cm2 sec-1), S the diffusion area (cm2), and t the duration of deployment (sec).</li>
	<li>Compare CDGT of Pu determined by DGTs with total Pu concentration in the bulk water, as well as with other available speciation data.</li>
</ol>
9. Radiochemical Separation for the Determination of Total Pu in the Bulk Water
<ol>
	<li>Condition water sample
	<ol>
		<li>Pump water from the studied body of water through a 45 &#181;m membrane filter into a plastic recipient. Work with samples of 10 to 50 L for AMS measurements. Acidify the water to pH 2 with HNO3 immediately after sampling at the sampling site prior to transporting to the laboratory.</li>
	</ol>
	</li>
	<li>Precipitate Pu on iron hydroxides
	<ol>
		<li>In the laboratory introduce an overhead stirrer into the recipient. Spike the sample with Pu yield tracer. Use a spike of 1.00 ml of 242Pu tracer of 0.25 mBq ml-1 (1.7 pg ml-1) activity concentration for AMS measurements.</li>
		<li>Add FeCl3&#183;6H2O taking about 0.25 g per 10 L sample. After having agitated for 30 min, precipitate iron hydroxides with NH4OH at pH 8.</li>
	</ol>
	</li>
	<li>Second precipitation of Pu on iron hydroxides
	<ol>
		<li>Decant the supernatant from water sample from point 9.2.2. Recover the precipitate of iron hydroxides into a 2 L glass beaker, rinse the recipient with deionized water and combine the washouts with the sample.</li>
		<li>Dissolve the precipitate in ~100 ml 5 M HCl, heat to 90 &#176;C to decompose carbonates. Filter if necessary when the solution is cooled down. Re-precipitate iron hydroxides with NH4OH at pH 8.</li>
	</ol>
	</li>
	<li>Condition iron hydroxides for analysis
	<ol>
		<li>Decant the supernatant from the sample from point 9.3.2. Recover the precipitate of iron hydroxide into a centrifugation vessel. Centrifuge, discard the supernatant. Wash the precipitate with deionized water. Repeat 2-3 times.</li>
		<li>Dissolve the precipitate in 10 ml 8 M HNO3, submit to radiochemical separation of Pu as described previously in the sections 7.4-7.6.</li>
	</ol>
	</li>
</ol>
10. Prepare Samples for AMS Measurements
<ol>
	<li>Precipitate Pu on iron hydroxides
	<ol>
		<li>After radiochemical separation, dissolve the final sample in 0.5 ml 1 M HCl, transfer the sample with a plastic pipette into a 2.5 ml glass vial. Rinse the sample beaker twice with 0.5 ml 1 M HCl, transfer washouts to the same vial.</li>
		<li>Add 0.5 ml of 2 mg ml-1 Fe3+ stock solution to provide 1 mg of iron. Precipitate iron hydroxides adding few drops of concentrated NH4OH. Centrifuge and decant the supernatant.</li>
		<li>Wash the precipitate with deionized water, centrifuge and decant the supernatant. Dry the precipitate on the hot plate at 90 &#176;C.</li>
	</ol>
	</li>
	<li>Prepare target for AMS measurements
	<ol>
		<li>Bake the hydroxides precipitate from point 10.1.3 in a furnace for 2-3 hr at 650 &#176;C. Thoroughly mix with 3-4 mg of niobium metal powder and press into a Ti target holder for AMS measurements. 
		Note: We measured the samples with the compact (0.6 MV) AMS system &#8220;TANDY&#8221; at the Swiss Federal Institute of Technology (ETH Zurich) tuned for measurements of actinides15,16.</li>
	</ol>
	</li>
</ol>

<ol>
	<li>Kaplan, D. I., et al. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Influence+of+oxidation+states+on+plutonium+mobility+during+long-term+transport+through+an+unsaturated+subsurface+environment.">Influence of oxidation states on plutonium mobility during long-term transport through an unsaturated subsurface environment.</a> Environ. Sci. Technol. 38 (19), 5053-5058 (2004).</li><li>Taylor, D. M. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Environmental+plutonium+-+Creation+of+the+universe+to+twenty-first+century+mankind.">Environmental plutonium - Creation of the universe to twenty-first century mankind.</a> Plutonium in the Environment. 1, 1-14 (2001).</li><li>Maher, K., Bargar, J. R., Brown, G. E. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Environmental+Speciation+of+Actinides.">Environmental Speciation of Actinides.</a> Inorganic Chemistry. 52 (7), 3510-3532 (2013).</li><li>Kurosaki, H., Kaplan, D. I., Clark, S. B. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Impact+of+environmental+curium+on+plutonium+migration+and+isotopic+signatures.">Impact of environmental curium on plutonium migration and isotopic signatures.</a> Environ. Sci. Technol. 48 (23), 13985-13991 (2014).</li><li>Orlandini, K. A., Penrose, W. R., Nelson, D. M. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Pu(V)+as+the+stable+form+of+oxidized+plutonium+in+natural-waters.">Pu(V) as the stable form of oxidized plutonium in natural-waters.</a> Marine Chemistry. 18 (1), 49-57 (1986).</li><li>Kaplan, D. I., et al. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Eleven-year+field+study+of+Pu+migration+from+Pu+III,+IV,+and+VI+sources.">Eleven-year field study of Pu migration from Pu III, IV, and VI sources.</a> Environ. Sci. Technol. 40 (2), 443-448 (2006).</li><li>Morgenstern, A., Choppin, G. R. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Kinetics+of+the+oxidation+of+Pu(IV)+by+manganese+dioxide.">Kinetics of the oxidation of Pu(IV) by manganese dioxide.</a> Radiochim. Acta. 90 (2), 69-74 (2002).</li><li>Davison, W., Zhang, H. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=In-situ+speciation+measurements+of+trace+components+in+natural-waters+using+thin-film+gels.">In-situ speciation measurements of trace components in natural-waters using thin-film gels.</a> Nature. 367 (6463), 546-548 (1994).</li><li>Zhang, H., Davison, W. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Diffusional+characteristics+of+hydrogels+used+in+DGT+and+DET+techniques.">Diffusional characteristics of hydrogels used in DGT and DET techniques.</a> Anal. Chim. Acta. 398 (2-3), 329-340 (1999).</li><li>Cusnir, R., Steinmann, P., Bochud, F., Froidevaux, P. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=A+DGT+Technique+for+Plutonium+Bioavailability+Measurements.">A DGT Technique for Plutonium Bioavailability Measurements.</a> Environ. Sci. Technol. 48 (18), 10829-10834 (2014).</li><li>Froidevaux, P., Steinmann, P., Pourcelot, L. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Long-Term+and+Long-Range+Migration+of+Radioactive+Fallout+in+a+Karst+System.">Long-Term and Long-Range Migration of Radioactive Fallout in a Karst System.</a> Environ. Sci. Technol. 44 (22), 8479-8484 (2010).</li><li>Bajo, S., Eikenberg, J. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Preparation+of+a+stable+tracer+solution+of+plutonium+(IV).">Preparation of a stable tracer solution of plutonium (IV).</a> Radiochim. Acta. 91 (9), 495-497 (2003).</li><li>Saito, A., Roberts, R. A., Choppin, G. R. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Preparation+of+solutions+of+tracer+level+plutonium+(V).">Preparation of solutions of tracer level plutonium (V).</a> Anal. Chem. 57 (1), 390-391 (1985).</li><li>Bajo, S., Eikenberg, J. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Electrodeposition+of+actinides+for+alpha-spectrometry.">Electrodeposition of actinides for alpha-spectrometry.</a> Journal of Radioanalytical and Nuclear Chemistry. 242 (3), 745-751 (1999).</li><li>Dai, X. X., Christl, M., Kramer-Tremblay, S., Synal, H. A. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Ultra-trace+determination+of+plutonium+in+urine+samples+using+a+compact+accelerator+mass+spectrometry+system+operating+at+300+kV.">Ultra-trace determination of plutonium in urine samples using a compact accelerator mass spectrometry system operating at 300 kV.</a> Journal of Analytical Atomic Spectrometry. 27 (1), 126-130 (2012).</li><li>Christl, M., et al. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=The+ETH+Zurich+AMS+facilities:+Performance+parameters+and+reference+materials.">The ETH Zurich AMS facilities: Performance parameters and reference materials.</a> Nuclear Instruments and Methods in Physics Research B. 294, 29-38 (2013).</li><li>Blinova, O., et al. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Redox+interactions+of+Pu(V)+in+solutions+containing+different+humic+substances.">Redox interactions of Pu(V) in solutions containing different humic substances.</a> Journal of Alloys and Compounds. 444, 486-490 (2007).</li></ol>

The authors have nothing to disclose.

The DGT methodology described here for experiments with Pu using a diffusion cell provides a reliable approach for various studies on Pu redox species and their interactions with organic molecules, colloidal particles and simulated environmental systems. Further applications of DGTs for environmental measurements of Pu will contribute to our understanding of the bioavailability and the fate of this radionuclide in aquatic ecosystems.
Laboratory diffusion experiments
In order to perform a successful diffusion experiment with meaningful conclusions on Pu mobility and interactions regarding a specific chemical environment, well defined and controllable conditions must be provided. The adjustment of Pu oxidation states prior to experiment is essential to simplify the data interpretation as well as to simulate various biogeochemical behaviors of Pu redox species. The sensitivity of Pu species to pH variations makes buffering the solutions a must. Particular attention should be drawn to the diffusion cell features and setup: the use of non-sorbing Teflon polymer material avoids adsorption on the cell walls and allows a robust leakproof assembly, preventing loss of Pu from diffusing solutions during the experiment.
The initial Pu concentration to be introduced into the A compartment, as well as the sampling interval and the volume of each sample taken during the diffusion experiment depend on the analytical method available in the laboratory. Any available analytical method can be used for determination of Pu concentration in the samples from the diffusion cell, however this choice is tightly bound to the initial activity of Pu taken for the experiment. 10 Bq of 239Pu as recommended in this protocol (giving 100-140 mBq ml-1 or ~2&#215;10-13 mol ml-1) are sufficient to provide enough sensitivity for measurements by alpha-spectrometry and generally do not pose particular problems for radiation protection regulations. The initial concentration of Pu can be reduced if other, more sensitive, analytical techniques are available for Pu determination (e.g., mass-spectrometry). Sampling interval can be selected for each diffusion experiment, depending on Pu initial concentration, and the expected rate of diffusion through the PAM gel. In spite of the fact that the aliquots from diffusion experiments do not contain radionuclides other than Pu, the presence of mineral salts and of the MOPS buffer can interfere with analytical procedure, reducing the efficiency and the precision of quantitative analysis. Therefore it is preferable to perform a chemical separation of Pu on these samples.
The diffusion cell provides the best approach to study diffusion in the PAM gel since the gel is exposed directly to a well stirred solution. Thus, the effects of the diffusive boundary layer (DBL) at the gel surface are considered negligible. Good stirring of the solutions during a diffusion experiment is essential, allowing for minimization of the DBL effects. In the same time, one should proceed carefully in order to not disrupt the PAM gel.
Studies of Pu bioavailability in natural freshwaters
The results produced by this protocol show that measuring plutonium with DGT devices provides an efficient tool to study the bioavailability of plutonium in freshwater. DGT measurements yield time-average concentration of free and labile species, the two most important forms for biological uptake by living organisms. In addition, the kinetics of the interaction of Pu with organic matter can be investigated using gels of different thickness. The time necessary for Pu-NOM species to diffuse through the gel will allow for the most labile complexes to dissociate. DGT measurements can be complemented by ultrafiltration techniques, which yield the percentage of Pu colloidal species above a given size (e.g., 8 kDa). Pu colloidal species are usually considered as non-bioavailable species and are part of the Pu fraction not measurable using DGT.
At this point, the DGT devices were deployed only in freshwater of a karst spring of the Swiss Jura Mountains. Low environmental concentrations of Pu require a long-term deployment of DGT devices, which can encounter potential drawbacks. Biofouling of the DGT surface represents a significant drawback, increasing the DBL thickness and thus limiting the flux of Pu through the PAM gel. Binding phase of the DGTs exposed in marine waters or waters of high mineralization may be rapidly saturated with other trace metals, misrepresenting the data for accumulation of Pu. Determination of trace levels of environmental Pu requires a thorough radiochemical separation and very sensitive analytical methods. AMS measurements applied in this protocol are not widely available, but can be replaced by other mass-spectrometry techniques. However, a rigorous radiochemical separation is necessary to eliminate the isobaric interference 238U-H from naturally occurring uranium.
Equation 2 shows that the size of the DGT device is an essential parameter that can be tuned to increase the quantity of accumulated Pu during a given deployment time. Commercial gel strips are available only with a maximum surface of 6 cm x 22 cm. Therefore, the window of the DGT sampler has been increased to 105 cm2 (5 cm &#215; 21 cm), making possible to accumulate enough of Pu species for relatively short deployment times. The assembly of such a DGT sampler requires precision and particular consideration of the PAM gel sheet properties while manipulating. It is of fundamental importance to assemble gel layers into a smooth-faced uniform &#8220;sandwich&#8221; in order to provide a homogeneous flux of Pu species from the bulk water through the diffusive gel. Good water flow at the DGT surface is also an important parameter, yet it is mostly determined by flow conditions in the aquifer. It is recommended to place DGT devices for Pu measurements at about 45&#176; towards the direction of water flow in order to provide a steady water supply and minimize the effects of the DBL.
Diffusion coefficient employed in the equation 2 must be corrected if the temperature in the studied body of water is different from the temperature at which the diffusion coefficient was determined. Temperature effects on diffusion coefficients are given by Stokes-Einstein equation (equation 3): 
<img alt="Equation 3" src="/files/ftp_upload/53188/53188eq3.jpg" />&#160;&#160;&#160;&#160; (3) 
where D1 and D2 are diffusion coefficients (cm2 sec-1), &#951;1 and &#951;2 are viscosities (mPa sec) of water at temperatures T1 and T2 (K) respectively.
Currently, there is no method to investigate Pu speciation in pristine environment, except for thermodynamic calculations based on, e.g., pH and redox parameters. These parameters are only available for macro-components, such as carbonates, iron or manganese cations. Thus, Pu speciation is derived from these measurable species but does not represent a &#8220;real&#8221; measurement. Here we think that the diffusion in thin PAM gel film technique as presented in this paper is an important step in the resolution of the Pu speciation problem because it allows measuring in situ free and labile species and, possibly, evidencing plutonyl species. Although only a few DGT measurements of the environmental Pu in freshwaters have been undertaken so far, the obtained results are encouraging for further applications of the DGT technique for Pu speciation and bioavailability studies. Deployment of DGTs in organic-rich waters will potentially yield important information on Pu mobility and interactions in presence of NOM molecules. Interesting results should be expected from DGT measurements in contaminated marine environments, such as the coastal seas around the Sellafield nuclear reprocessing plant and the damaged Fukushima Daiichi nuclear power plant.

Plutonium is an artificial radionuclide present in the environment as a result of the global fallout following the nuclear bomb tests and nuclear accidents. The redox chemistry of plutonium has important implications for its migration and biogeochemical cycling in environmental aquatic systems1. Plutonium has a complex chemistry and can exist in four oxidation states (III, IV, V, VI) at the same time. Therefore, the distribution of redox species of plutonium in natural waters is extremely sensitive to local chemical environment2,3. The oxidation state of plutonium also depends on the origin of the source &#8212; this statement being mostly relevant for contaminated environments and disposal sites. Reduced plutonium species (+III and +IV) are found predominately in anoxic environments and originate from global fallout and stocked waste effluents, while higher oxidation states (+V and +VI) can be found among decay products of other actinides and in oxic environments4.
The mobility and the environmental behavior of plutonium can be predicted to some extent from the redox speciation. Plutonium in +III and +IV oxidation states exists predominately in solid phase and has increased capacity to sorb to inorganic colloids and naturally occurring organic matter (NOM) molecules. Plutonium in +III and +IV oxidation states is considered to be less mobile. More soluble oxidized forms of plutonium (+V and +VI, +V being most likely)5 can potentially contribute to a higher biological transfer to aquatic organisms due to higher mobility. Nevertheless, in presence of NOM, particularly of humic acid, Pu(V) is being reduced17, shifting the partitioning several orders of magnitude in favor of precipitation. Despite the fact that the reduction rate of Pu(V) to Pu(IV) is 4 to 5 orders of magnitude faster than the reverse reaction, remobilization of Pu(IV) under oxidizing conditions may also take place1. Recent experimental data on mineral sediments amended with Pu(IV) and subjected to natural oxidizing conditions have demonstrated that the concentration of soluble Pu in aqueous phase increased over time1,6. The authors explain it by oxidative desorption of Pu(IV) and formation of more soluble Pu(V) and Pu(VI) species. Oxidation of Pu(IV) may also occur due to naturally encountered manganese oxides7. These observations are important for bioavailability modeling and environmental risk assessment of waste disposal and contaminated sites.
Studies on bioavailability and speciation of plutonium is a challenging task in both laboratory and in-situ conditions. Low environmental concentrations, the variability of redox species and the interactions with natural colloids make it difficult to simulate the biogeochemical behavior of plutonium. The technique of diffusive gradients in thin films (DGT) based on the diffusion of free and labile contaminant species through a polyacrylamide (PAM) gel is widely used for environmental measurements of trace elements8. A DGT sampler represents a three-layer device made of a binding phase (for the majority of trace metals it is Chelex resin contained in the PAM gel), diffusive gel layer (PAM gel of varying thickness) and a filter membrane protecting the gel and holding the assembly together. Thin films of polyacrylamide gel, consisting of 85% of water, enable free and labile complex species to diffuse more rapidly than plutonium bound to large NOM molecules or natural colloidal particles. A set-up designed to study plutonium diffusion in thin PAM gel films in laboratory conditions is called a diffusion cell9.
A diffusion cell is a two-compartment vessel where two separate compartments are interconnected by an opening of a given surface. The opening, i.e., the window between the two chambers contains a disc of diffusion gel of a given thickness. We constructed a Teflon cell with two 100 ml compartments and a circular diffusion window 1.7 cm in diameter. One compartment is removable, facilitating the assembly. A 0.5 cm wide groove carved around the diffusion window on the fixed compartment serves to place the diffusive gel disc. The groove depth should be similar to PAM gel thickness intended for use. We choose to work with a 0.39 mm PAM gel, thus the groove depth in our diffusion cell is 0.39 mm. A detailed picture of the diffusion cell is given in Figure 1.
When a solution initially containing plutonium is placed into one compartment (A), diffusing Pu species will establish a concentration gradient in the gel and will start to accumulate in the second compartment (B), initially containing a solution of the same chemical composition without Pu. The initial concentration of Pu species in compartment A is defined such that it remains constant or changes very little (by 1%-2% at most) throughout the diffusion experiment. Plotting the amount of diffused Pu versus time provides a means to analyze the mobility of Pu species prevailing in the different simulated environmental conditions. Diffusion in thin films provides a valuable alternative for studies on Pu mobility and speciation and can be successfully applied in field conditions10. One can replace the diffusion cell by a passive sampler, manufactured with the PAM diffusive gel and Chelex resin as the binding phase, which serves to accumulate diffusing Pu species. Such a sampler can be exposed in field conditions &#8212; the amount of Pu accumulated in the resin will be indicative of the speciation and the bioavailability of Pu in the respective environment10.
In this work, we used a diffusion cell to investigate the mobility of Pu(IV) and Pu(V) species and their interactions with NOM in laboratory conditions. Furthermore, we applied large passive DGT samplers of a surface of 105 cm2 to study the bioavailability of Pu in a karstic spring of the Swiss Jura Mountains (Venoge River) where a significant fraction of Pu was found in the intracellular parts of aquatic mosses in a previous work11. Because of the very low level of plutonium present in this pristine environment, accelerator-based mass spectrometry (AMS) techniques available at ETH Zurich were used to measure plutonium isotopes.

<table border="0" cellpadding="0" cellspacing="0">
	<tbody>
		<tr>
			<td>239Pu tracer</td>
			<td>CEA</td>
			<td></td>
			<td>Source PU239-ELSC10</td>
		</tr>
		<tr>
			<td>242Pu tracer</td>
			<td>LNSIRR</td>
			<td></td>
			<td>Source Pu242 N&#176; 790 from Laboratory for National Standards of Ionizing Radiation of Russia</td>
		</tr>
		<tr>
			<td>25 ml Beakers</td>
			<td></td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Pipette</td>
			<td>Socorex</td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Disposable plastic pipettes</td>
			<td>Semadeni</td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>20 ml Plastic scintillation vial</td>
			<td>Semadeni</td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Aluminium foil</td>
			<td></td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Hot plate</td>
			<td></td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Tweezers</td>
			<td></td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Actinide exchange resin - TEVA - B</td>
			<td>Triskem</td>
			<td>TE-B50-A</td>
			<td></td>
		</tr>
		<tr>
			<td>Actinide exchange resin - TEVA - R cartridges</td>
			<td>Triskem</td>
			<td>TE-R10-S</td>
			<td></td>
		</tr>
		<tr>
			<td>1 ml Pipette tips</td>
			<td>Socorex</td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>PAM gel strip 6&#215;21 cm</td>
			<td>DGT Research Ltd</td>
			<td></td>
			<td>0.39 mm and 0.78 mm thickness / www.dgtresearch.com</td>
		</tr>
		<tr>
			<td>Chelex gel strip 6&#215;21 cm</td>
			<td>DGT Research Ltd</td>
			<td></td>
			<td>0.40 mm thickness / www.dgtresearch.com</td>
		</tr>
		<tr>
			<td>Diffusion cell</td>
			<td></td>
			<td></td>
			<td>Fabricated / in-house workshop</td>
		</tr>
		<tr>
			<td>&#216; 27 mm Punch</td>
			<td></td>
			<td></td>
			<td>Fabricated / in-house workshop</td>
		</tr>
		<tr>
			<td>Plastic tray</td>
			<td></td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>DGT set-up</td>
			<td></td>
			<td></td>
			<td>Fabricated / in-house workshop</td>
		</tr>
		<tr>
			<td>Membrane filter</td>
			<td>PALL Corporation</td>
			<td></td>
			<td>HT-450 Tuffryn Polysulfone Membrane Disc Filter 0.45 &#956;m / 145 &#956;m thickness</td>
		</tr>
		<tr>
			<td>Nitric acid&#160;</td>
			<td>Carlo Erba</td>
			<td align="right">408025</td>
			<td></td>
		</tr>
		<tr>
			<td>Sulfuric acid</td>
			<td>Sigma-Aldrich</td>
			<td align="right">84720</td>
			<td></td>
		</tr>
		<tr>
			<td>Hydrocloric acid</td>
			<td>Carlo Erba</td>
			<td align="right">403981</td>
			<td></td>
		</tr>
		<tr>
			<td>Hydriodic acid</td>
			<td>Merck</td>
			<td align="right">100341</td>
			<td></td>
		</tr>
		<tr>
			<td>Potassium permanganate</td>
			<td>Merck</td>
			<td align="right">105082</td>
			<td></td>
		</tr>
		<tr>
			<td>Sodium hydrogen sulfate</td>
			<td>Merck</td>
			<td align="right">106352</td>
			<td></td>
		</tr>
		<tr>
			<td>Sodium sulfate</td>
			<td>Merck</td>
			<td align="right">106647</td>
			<td></td>
		</tr>
		<tr>
			<td>Sodium nitrate</td>
			<td>Sigma-Aldrich</td>
			<td align="right">31440</td>
			<td></td>
		</tr>
		<tr>
			<td>Sodium nitrite</td>
			<td>Fluka</td>
			<td align="right">71759</td>
			<td></td>
		</tr>
		<tr>
			<td>Sodium acetate</td>
			<td>Merck</td>
			<td align="right">106281</td>
			<td></td>
		</tr>
		<tr>
			<td>Ammonium oxalate</td>
			<td>Fluka</td>
			<td align="right">9900</td>
			<td></td>
		</tr>
		<tr>
			<td>Bis-(2-ethyl hexyl) phosphoric acid (HEDHP)</td>
			<td>Merck</td>
			<td align="right">177092</td>
			<td></td>
		</tr>
		<tr>
			<td>2-thenoyltrifluoroacetone (TTA)</td>
			<td>Fluka</td>
			<td align="right">88300</td>
			<td></td>
		</tr>
		<tr>
			<td>MOPS buffer</td>
			<td>Sigma-Aldrich</td>
			<td>M9381</td>
			<td>MOPS sodium salt</td>
		</tr>
		<tr>
			<td>Cyclohexane</td>
			<td>Carlo Erba</td>
			<td></td>
			<td></td>
		</tr>
		<tr>
			<td>Humic acid</td>
			<td></td>
			<td></td>
			<td>Extracted from an organic-rich soil of an Alpine Valley, freeze-dried, MW 5-40 kDa</td>
		</tr>
		<tr>
			<td>NH4OH</td>
			<td>Carlo Erba</td>
			<td align="right">419943</td>
			<td></td>
		</tr>
		<tr>
			<td>FeCl3&#183;H2O</td>
			<td>Sigma-Aldrich</td>
			<td align="right">44944</td>
			<td></td>
		</tr>
	</tbody>
</table>

speciation and bioavailability measurements of environmental plutonium using diffusion in thin films

The biological uptake of plutonium (Pu) in aquatic ecosystems is of particular concern since it is an alpha-particle emitter with long half-life which can potentially contribute to the exposure of biota and humans. The diffusive gradients in thin films technique is introduced here for in-situ measurements of Pu bioavailability and speciation. A diffusion cell constructed for laboratory experiments with Pu and the newly developed protocol make it possible to simulate the environmental behavior of Pu in model solutions of various chemical compositions. Adjustment of the oxidation states to Pu(IV) and Pu(V) described in this protocol is essential in order to investigate the complex redox chemistry of plutonium in the environment. The calibration of this technique and the results obtained in the laboratory experiments enable to develop a specific DGT device for in-situ Pu measurements in freshwaters. Accelerator-based mass-spectrometry measurements of Pu accumulated by DGTs in a karst spring allowed determining the bioavailability of Pu in a mineral freshwater environment. Application of this protocol for Pu measurements using DGT devices has a large potential to improve our understanding of the speciation and the biological transfer of Pu in aquatic ecosystems.

Diffusion experiments
Plotting the activities of 239Pu diffused into the B compartment of the diffusion cell versus time gives a visual representation of the flux of the 239Pu species diffusing through the PAM gel. Diffusion coefficients calculated from these plots according to equation 1 provide an additional means to compare mobility of different 239Pu redox species in various chemical environments (Figure 2). Figure 5 illustrates the diffusion experiments with Pu(IV) and Pu(IV)-Pu(V) mixed species, respectively, in the MOPS buffer and in presence of 20 ppm of HA. A comparison of these plots shows that Pu(V) is significantly more mobile than Pu(IV).This is particularly valid for Pu(IV) and Pu(V) when HA (MW 5-40 kDa in our experiments, characterized in the SI by Cusnir et al.)10 is added as complexing molecules. Pu(V) source solution prepared according to the protocol described in this paper contains predominately Pu(V) species. Liquid phase extraction with HDEHP at the end of the diffusion experiment in the MOPS buffered solution found 80% &#177; 10% of Pu(V). The chemical yield of this extraction is 80%. The solution with Pu(V) in presence of 20 ppm of HA was equilibrated during 24 hr and Pu(V) fraction in this model solution was 35% &#177; 10%.
Studies on Pu bioavailability in natural freshwaters
Several DGT devices constructed in our laboratory were successfully exposed for periods of two to three weeks in a karst spring of the Swiss Jura Mountains. This is a mineral spring with the pH of the water in the range of 6.5-7.5, conductivity above 400 &#181;S cm-1 and saturated with oxygen. These experiments demonstrated good applicability and robustness of the gel assemblies with no trace of biofouling, possibly also because of the low temperature of the spring (7 &#176;C). DGTs retrieved after the deployments were well preserved, with gel layers intact, conserving the initial form and visual appearance. Pu accumulated by DGTs was analyzed by AMS. AMS provides considerable advantages over other analytical techniques: it is highly sensitive (down to sub-fg levels), and requires much lower initial sample amount than alpha-spectrometry or ICP-MS techniques. In addition, molecular isobaric interferences, such as the uranium hydride (238U-H), or other molecules are efficiently suppressed during the AMS measurement and do not interfere with the 239Pu detection. For some technical reasons (most probably a contamination with 239Pu during chemical separations), we were not able to use the data for 239Pu for the first applications of DGTs in the field. Nevertheless, the 240Pu results were unbiased. Thus, we calculated the 239Pu content from the measured 240Pu, taking 0.18 as 240Pu/239Pu atomic ratio for fallout plutonium. The results are summarized in Table 1.
239Pu concentrations measured in bulk water samples are similar to concentrations previously reported for this aquifer (1-7 &#181;Bq L-1)11. Furthermore, 239Pu concentrations calculated from DGT measurements are similar within the uncertainties of the measurement. Since DGTs accumulate only free and labile Pu species, one can estimate the fraction of bioavailable Pu in this water. Data given in Table 1 indicate that all the 239Pu species present in the bulk water are found in a bioavailable form. This is an interesting result in the light of previous findings11, which have revealed the predominant accumulation of 239+240Pu in the intracellular fraction of the aquatic mosses growing in the spring compared to 241Am and 90Sr. The authors11 suggested that the enhanced mobility of Pu in this natural aquifer was due to formation of a soluble carbonate Pu complex, possibly as a Pu(V) plutonyl form, similar to naturally occurring uranyl-carbonate complex. Water of the Venoge spring is hard water, with high carbonate concentration and very low NOM content (about 1 ppm).
<img alt="Figure 1" src="/files/ftp_upload/53188/53188fig1.jpg" /> 
Figure 1. Diffusion cell used for experiments on Pu diffusion through the PAM gel. The groove thickness 0.5 cm, the groove depth 0.39 mm. <a href="https://www.jove.com/files/ftp_upload/53188/53188fig1large.jpg" target="_blank">Please click here to view a larger version of this figure.</a>
<img alt="Figure 2" src="/files/ftp_upload/53188/53188fig2.jpg" /> 
Figure 2. Snapshot of the Excel Worksheet used for calculations of the diffusion coefficient. <a href="https://www.jove.com/files/ftp_upload/53188/53188fig2large.jpg" target="_blank">Please click here to view a larger version of this figure.</a>
<img alt="Figure 3" src="/files/ftp_upload/53188/53188fig3.jpg" /> 
Figure 3. Large-surface DGT device for environmental Pu speciation measurements. Parts of the DGT device &#8212; the bottom plate and the cover frame &#8212; depicted on the left, the assembly with crew holes on the right. <a href="https://www.jove.com/files/ftp_upload/53188/53188fig3large.jpg" target="_blank">Please click here to view a larger version of this figure.</a>
<img alt="Figure 4" src="/files/ftp_upload/53188/53188fig4.jpg" /> 
Figure 4. DGT sampler devices fixed in the holder (left) exposed in the Venoge spring (right) for Pu bioavailability measurements. <a href="https://www.jove.com/files/ftp_upload/53188/53188fig4large.jpg" target="_blank">Please click here to view a larger version of this figure.</a>
<img alt="Figure 5" src="/files/ftp_upload/53188/53188fig5.jpg" /> 
Figure 5. Plot of the 239Pu diffused into B compartment of the diffusion cell in different chemical environments. Experimental data points are given for 239Pu(IV) and 239Pu(V), respectively, in MOPS buffer as well as for 239Pu(IV)-239Pu(V) mixed species (35% &#177; 10% of Pu(V)) in the presence of HA. The line shown for 239Pu(IV)-HA has been calculated using a diffusion coefficient of 0.50&#215;10-6 cm2 sec-1 determined previously10. Diffusion coefficients calculated from equation 1 are: Pu(IV) in MOPS buffer &#8212; 2.29&#215;10-6 cm2 sec-1, Pu(V) in MOPS buffer &#8212; 3.50&#215;10-6 cm2 sec-1, Pu(IV) - Pu(V) with HA &#8212; 0.92&#215;10-6 cm2 sec-1. From top to bottom: Pu(V) in MOPS buffer (red open circle), Pu(IV) in the MOPS buffer (blue open triangles), Pu(IV) - Pu(V) in presence of 20 ppm of HA (green open squares), Pu(IV) in presence of 20 ppm of HA (brown open diamonds). <a href="https://www.jove.com/files/ftp_upload/53188/53188fig5large.jpg" target="_blank">Please click here to view a larger version of this figure.</a>
<table border="0">
	<tbody>
		<tr>
			<td>Sample type</td>
			<td>Number of measurements</td>
			<td>239Pu concentration, &#956;Bq L-1</td>
		</tr>
		<tr>
			<td>Bulk water</td>
			<td>2</td>
			<td>1.9 &#177; 0.55</td>
		</tr>
		<tr>
			<td>DGT 0.39 mm</td>
			<td>2</td>
			<td>1.74 &#177; 0.9</td>
		</tr>
		<tr>
			<td>DGT 0.78 mm</td>
			<td>1</td>
			<td>1.79 &#177; 0.9</td>
		</tr>
	</tbody>
</table>
Table 1. Representative results for 239Pu measurements by AMS in the bulk water and DGT samplers. 239Pu in the bulk water was co-precipitated from 20 L of water with iron hydroxides, extracted on the actinide-specific exchange resin and measured by AMS. 239Pu concentrations for DGT measurements calculated using equation 2 and diffusion coefficient for Pu(IV). Uncertainties for k=2; u(95).

Watch this Scientific Journal Video about Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films at JoVE.com

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films

The technique of diffusive gradients in thin films (DGT) is proposed for speciation studies of plutonium. This protocol describes diffusion experiments probing the behavior of Pu(IV) and Pu(V) in presence of organic matter. DGTs deployed in a karstic spring allow assessment of the bioavailability of Pu.

The biological uptake of plutonium (Pu) in aquatic ecosystems is of particular concern since it is an alpha-particle emitter with long half-life which can ...

speciation-bioavailability-measurements-environmental-plutonium-using

Research

Education

JoVE Journal

JoVE Core

Biology

Engineering

Evolution

Speciation and Diversity

SCIENTISTS IN ACTION

11.2K ビュー.  Lausanne University Hospital. 薄膜における拡散勾配（DGT）の技術は、プルトニウムの分化の研究のために提案されています。このプロトコルは、有機物の存在下でのPu（IV）とPu（V）の動作をプロービング拡散実験について説明します。カルスト春に配備DGTSはプルトニウムの生物学的利用能の評価を可能にします。 

ビデオ: Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films

Formation of Thick Dense Yttrium Iron Garnet Films Using Aerosol Deposition

Aerosol deposition (AD) is a thick-film deposition process that can produce layers up to several hundred micrometers thick with densities greater than 95% of the bulk. The primary advantage of AD is that the deposition takes place entirely at ambient temperature; thereby enabling film growth in material systems with disparate melting temperatures. This report describes in detail the processing steps for preparing the powder and for performing AD using the custom-built system. Representative characterization results are presented from scanning electron microscopy, profilometry, and ferromagnetic resonance for films grown in this system. As a representative overview of the capabilities of the system, focus is given to a sample produced following the described protocol and system setup. Results indicate that this system can successfully deposit 11 &#181;m thick yttrium iron garnet films that are &#160;&#62; 90% of the bulk density during a single 5 min deposition run. A discussion of methods to afford better control of the aerosol and particle selection for improved thickness and roughness variations in the film is provided.

This report describes the use of a custom-built system to perform aerosol deposition of thick films of yttrium iron garnet onto sapphire substrates at RT. The deposited films are characterized using scanning electron microscopy, profilometry, and ferromagnetic resonance to give a representative overview of the capabilities of the technique.

Aerosol deposition (AD) is a thick-film deposition process that can produce layers up to several hundred micrometers thick with densities greater than 95% ...

Detection and Recovery of Palladium, Gold and Cobalt Metals from the Urban Mine Using Novel Sensors/Adsorbents Designated with Nanoscale Wagon-wheel-shaped Pores

Developing low-cost, efficient processes for recovering and recycling palladium, gold and cobalt metals from urban mine remains a significant challenge in industrialized countries. Here, the development of optical mesosensors/adsorbents (MSAs) for efficient recognition and selective recovery of Pd(II), Au(III), and Co(II) from urban mine was achieved. A simple, general method for preparing MSAs based on using high-order mesoporous monolithic scaffolds was described. Hierarchical cubic Ia3d wagon-wheel-shaped MSAs were fabricated by anchoring chelating agents (colorants) into three-dimensional pores and micrometric particle surfaces of the mesoporous monolithic scaffolds. Findings show, for the first time, evidence of controlled optical recognition of Pd(II), Au(III), and Co(II) ions and a highly selective system for recovery of Pd(II) ions (up to ~95%) in ores and industrial wastes. Furthermore, the controlled assessment processes described herein involve evaluation of intrinsic properties (e.g., visual signal change, long-term stability, adsorption efficiency, extraordinary sensitivity, selectivity, and reusability); thus, expensive, sophisticated instruments are not required. Results show evidence that MSAs will attract worldwide attention as a promising technological means of recovering and recycling palladium, gold and cobalt metals.

Because of the importance and extensive use of palladium, gold and cobalt metals in high-technology equipment, their recovery and recycling constitute an important industrial challenge. The metal recovery system described herein is a simple, low-cost means for the effective detection, removal, and recovery of these metals from the urban mine.

Developing low-cost, efficient processes for recovering and recycling palladium, gold and cobalt metals from urban mine remains a significant challenge in ...

Indirect Fabrication of Lattice Metals with Thin Sections Using Centrifugal Casting

One of the typical methods to manufacture 3D lattice metals is the direct-metal additive manufacturing (AM) process such as Selective Laser Melting (SLM) and Electron Beam Melting (EBM). In spite of its potential processing capability, the direct AM method has several disadvantages such as high cost, poor surface finish of final products, limitation in material selection, high thermal stress, and anisotropic properties of parts. We propose a cost-effective method to manufacture 3D lattice metals. The objective of this study is to provide a detailed protocol on fabrication of 3D lattice metals having a complex shape and a thin wall thickness; e.g., octet truss made of Al and Cu alloys having a unit cell length of 5 mm and a cell wall thickness of 0.5 mm. An overall experimental procedure is divided into eight sections: (a) 3D printing of sacrificial patterns (b) melt-out of support materials (c) removal of residue of support materials (d) pattern assembly (e) investment (f) burn-out of sacrificial patterns (g) centrifugal casting (h) post-processing for final products. The suggested indirect AM technique provides the potential to manufacture ultra-lightweight lattice metals; e.g., lattice structures with Al alloys. It appears that the process parameters should be properly controlled depending on materials and lattice geometry, observing the final products of octet truss metals by the indirect AM technique.

An indirect additive manufacturing method combining a 3D printing of polymers with a centrifugal casting is outlined for manufacturing 3D octet truss metals (Al and Cu alloys) having a unit cell length of 5 mm with a wall thickness of 0.5 mm.

One of the typical methods to manufacture 3D lattice metals is the direct-metal additive manufacturing (AM) process such as Selective Laser Melting (SLM) ...

Electrospray Deposition of Uniform Thickness Ge23Sb7S70 and As40S60 Chalcogenide Glass Films

Solution-based electrospray film deposition, which is compatible with continuous, roll-to-roll processing, is applied to chalcogenide glasses. Two chalcogenide compositions are demonstrated: Ge23Sb7S70 and As40S60, which have both been studied extensively for planar mid-infrared (mid-IR) microphotonic devices. In this approach, uniform thickness films are fabricated through the use of computer numerical controlled (CNC) motion. Chalcogenide glass (ChG) is written over the substrate by a single nozzle along a serpentine path. Films were subjected to a series of heat treatments between 100 &#176;C and 200 &#176;C under vacuum to drive off residual solvent and densify the films. Based on transmission Fourier transform infrared (FTIR) spectroscopy and surface roughness measurements, both compositions were found to be suitable for the fabrication of planar devices operating in the mid-IR region. Residual solvent removal was found to be much quicker for the As40S60 film as compared to Ge23Sb7S70. Based on the advantages of electrospray, direct printing of a gradient refractive index (GRIN) mid-IR transparent coating is envisioned, given the difference in refractive index of the two compositions in this study.

Electrospray Deposition of Uniform Thickness Ge23Sb7S70 and As40S60 Chalcogenide Glass Films

A method of uniform thickness solution-derived chalcogenide glass film deposition is demonstrated using computer numerical controlled motion of a single-nozzle electrospray.

Solution-based electrospray film deposition, which is compatible with continuous, roll-to-roll processing, is applied to chalcogenide glasses. Two ...

In Situ Monitoring of the Accelerated Performance Degradation of Solar Cells and Modules: A Case Study for Cu(In,Ga)Se2 Solar Cells

The levelized cost of electricity (LCOE) of photovoltaic (PV) systems is determined by, among other factors, the PV module reliability. Better prediction of degradation mechanisms and prevention of module field failure can consequently decrease investment risks as well as increase the electricity yield. An improved knowledge level can for these reasons significantly decrease the total costs of PV electricity. 
In order to better understand and minimize the degradation of PV modules, the occurring degradation mechanisms and conditions should be identified. This should preferably happen under combined stresses, since modules in the field are also simultaneously exposed to multiple stress factors. Therefore, two 'Combined Stress test with in situ measurement' setups have been designed and constructed. These setups allow the simultaneous use of humidity, temperature, illumination, and electrical biases as independently controlled stress factors on solar cells and minimodules. The setups also allow real-time monitoring of the electrical properties of these samples. This protocol presents these setups and describes the experimental possibilities. Moreover, results obtained with these setups are also presented: various examples about the influence of both deposition and degradation conditions on the stability of thin film Cu(In,Ga)Se2 (CIGS) as well as Cu2ZnSnSe4 (CZTS) solar cells are described. Results on the temperature dependency of CIGS solar cells are also presented.

In Situ Monitoring of the Accelerated Performance Degradation of Solar Cells and Modules: A Case Study for CuIn,GaSe2 Solar Cells

Two &#39;Combined Stress test with in situ measurement&#39; setups, which allow real-time monitoring of accelerated degradation of solar cells and modules, were designed and constructed. These setups allow the simultaneous use of humidity, temperature, electrical biases, and illumination as independently controlled stress factors. The setups and various experiments executed are presented.

The levelized cost of electricity (LCOE) of photovoltaic (PV) systems is determined by, among other factors, the PV module reliability. Better prediction ...

Fabrication of Ultra-thin Color Films with Highly Absorbing Media Using Oblique Angle Deposition

Ultra-thin film structures have been studied extensively for use as optical coatings, but performance and fabrication challenges remain.&#160; We present an advanced method for fabricating ultra-thin color films with improved characteristics. The proposed process addresses several fabrication issues, including large area processing. Specifically, the protocol describes a process for fabricating ultra-thin color films using an electron beam evaporator for oblique angle deposition of germanium (Ge) and gold (Au) on silicon (Si) substrates.&#160; Film porosity produced by the oblique angle deposition induces color changes in the ultra-thin film. The degree of color change depends on factors such as deposition angle and film thickness. Fabricated samples of the ultra-thin color films showed improved color tunability and color purity. In addition, the measured reflectance of the fabricated samples was converted into chromatic values and analyzed in terms of color. Our ultra-thin film fabricating method is expected to be used for various ultra-thin film applications such as flexible color electrodes, thin film solar cells, and optical filters. Also, the process developed here for analyzing the color of the fabricated samples is broadly useful for studying various color structures.

We present a detailed method for fabricating ultra-thin color films with improved characteristics for optical coatings. The oblique angle deposition technique using an electron beam evaporator allows improved color tunability and purity. Fabricated films of Ge and Au on Si substrates were analyzed by reflectance measurements and color information conversion.

Ultra-thin film structures have been studied extensively for use as optical coatings, but performance and fabrication challenges remain.&#160; We present ...

The Diffusion of Passive Tracers in Laminar Shear Flow

A simple method to experimentally observe and measure the dispersion of a passive tracer in a laminar fluid flow is described. The method consists of first injecting fluorescent dye directly into a pipe filled with distilled water and allowing it to diffuse across the cross-section of the pipe to obtain a uniformly distributed initial condition. Following this period, the laminar flow is activated with a programmable syringe pump to observe the competition of advection and diffusion of the tracer through the pipe. Asymmetries in the tracer distribution are studied and correlations between the pipe cross-section and the shape of the distribution is shown: thin channels (aspect ratio &#60;&#60; 1) produce tracers arriving with sharp fronts and tapering tails (front-loaded distributions), while thick channels (aspect ratio ~1) present the opposite behavior (back-loaded distributions). The experimental procedure is applied to capillary tubes of various geometries and is particularly relevant to microfluidic applications by dynamical similarity.

A protocol for the study of the diffusion of passive tracers in laminar pressure-driven flow is presented. The procedure is applicable to various capillary pipe geometries.

A simple method to experimentally observe and measure the dispersion of a passive tracer in a laminar fluid flow is described. The method consists of ...

Film Control to Study Contributions of Waves to Droplet Impact Dynamics on Thin Flowing Liquid Films

Droplet impact is a very common phenomenon in nature and attracts attention due to its aesthetic fascination and wide-ranging applications. Previous studies on flowing liquid films have neglected the contributions of spatial structures of waves to the impact outcome, while this has recently been shown to have a significant influence on the drop impact dynamics. In this report, we outline a step-by-step procedure to investigate the effect of periodic inlet forcing of a flowing liquid film leading to the production of spatiotemporally regular wave structures on drop impact dynamics. A function generator in connection with a solenoid valve is used to excite these spatiotemporally regular wave structures on the film surface while the impact dynamics of uniform-sized droplets are captured using a high-speed camera. Three distinct regions are then studied; viz. the capillary wave region preceding the large wave peak, the flat film region, and the wave hump region. The effects of important dimensionless quantities such as film Reynolds, drop Weber and Ohnesorge numbers parameterized by the film flow rate, drop speed, and drop size are also examined. Our results show interesting, hitherto undiscovered dynamics brought about by this application of film inlet forcing of the flowing film for both low and high inertia drops.

A protocol to study the contributions of waves to droplet impact dynamics on flowing liquid films is presented.

Droplet impact is a very common phenomenon in nature and attracts attention due to its aesthetic fascination and wide-ranging applications. Previous ...

Determining Tribocorrosion Rate and Wear-Corrosion Synergy of Bulk and Thin Film Aluminum Alloys

The increasing complexity and severity of service conditions in areas, such as aerospace and marine industries, nuclear systems, microelectronics, batteries, and biomedical devices, etc., impose great challenges on the reliable performance of alloys exposed to extreme conditions where mechanical and electrochemical attack co-exist. Finding ways for alloys to mitigate the combined attack of wear and corrosion (i.e., tribocorrosion) under such extreme conditions is thus highly critical for improving their reliability and service lifetime when used in such conditions. The challenge lies in the fact that wear and corrosion are not independent of each other, but rather work synergistically to accelerate the total material loss. Thus, a reliable method to evaluate the tribocorrosion resistance of metals and alloys is needed. Here, a protocol for measuring the tribocorrosion rate and wear-corrosion synergy of Al-based bulk and thin film samples in a corrosive environment under room temperature is presented.

Here, we present a protocol to measure the tribocorrosion rate and wear-corrosion synergy of thin film and bulk Al alloys in simulated sea water at room temperature.

The increasing complexity and severity of service conditions in areas, such as aerospace and marine industries, nuclear systems, microelectronics, ...

Plasma-Assisted Molecular Beam Epitaxy Growth of Mg3N2 and Zn3N2 Thin Films

This article describes a procedure for growing Mg3N2 and Zn3N2 films by plasma-assisted molecular beam epitaxy (MBE). The films are grown on 100 oriented MgO substrates with N2 gas as the nitrogen source. The method for preparing the substrates and the MBE growth process are described. The orientation and crystalline order of the substrate and film surface are monitored by the reflection high energy electron diffraction (RHEED) before and during growth. The specular reflectivity of the sample surface is measured during growth with an Ar-ion laser with a wavelength of 488 nm. By fitting the time dependence of the reflectivity to a mathematical model, the refractive index, optical extinction coefficient, and growth rate of the film are determined. The metal fluxes are measured independently as a function of the effusion cell temperatures using a quartz crystal monitor. Typical growth rates are 0.028 nm/s at growth temperatures of 150 &#176;C and 330 &#176;C for Mg3N2 and Zn3N2 films, respectively.

Plasma-Assisted Molecular Beam Epitaxy Growth of Mg3N2 and Zn3N2 Thin Films

This article describes the growth of epitaxial films of Mg3N2 and Zn3N2 on MgO substrates by plasma-assisted molecular beam epitaxy with N2 gas as the nitrogen source and optical growth monitoring.

This article describes a procedure for growing Mg3N2 and Zn3N2 films by plasma-assisted molecular beam epitaxy (MBE). The films are grown on 100 oriented ...