Name: microplot design and plant and soil sample preparation for 15nitrogen analysis
Uploaded: 2020-05-10T14:00:00
Description: Watch this Scientific Journal Video about Microplot Design and Plant and Soil Sample Preparation for 15Nitrogen Analysis at JoVE.com

The authors acknowledge the support of the Minnesota Corn Research &#38; Promotion Council, the Hueg-Harrison Fellowship, and the Minnesota&#39;s Discovery, Research and InnoVation Economy (MnDRIVE) Fellowship.

1. Field site description
NOTE: When performing 15N tracer field trials, selected sites should minimize variation due to soil, topography, and physical features5. Cross-contamination may occur following lateral soil movement due to slope, wind or water translocation, or tillage while the vertical distribution of soil N may be impacted by subsurface water flow and tile-drainage6.
<ol>
	<li>Describe the experimental field site includin...

<ol>
	<li>Sharp, Z. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=.">.</a> Principles of Stable Isotope Geochemistry. , (2017).</li><li>Van Cleemput, O., Zapata, F., Vanlauwe, B. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Guidelines+on+Nitrogen+Management+in+Agricultural+Systems.">Guidelines on Nitrogen Management in Agricultural Systems.</a> Guidelines on Nitrogen Management in Agricultural Systems. 29 (29), 19 (2008).</li><li>Hauck, R. D., Meisinger, J. J., Mulvaney, R. L. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Practical+considerations+in+the+use+of+nitrogen+tracers+in+agricultural+and+environmental+research.">Practical considerations in the use of nitrogen tracers in agricultural and environmental research.</a> Methods of Soil Analysis: Part 2-Microbiological and Biochemical Properties. , 907-950 (1994).</li><li>Bedard-Haughn, A., Van Groenigen, J. W., Van Kessel, C. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Tracing+15N+through+landscapes:+Potential+uses+and+precautions.">Tracing 15N through landscapes: Potential uses and precautions.</a> Journal of Hydrology. 272 (1-4), 175-190 (2003).</li><li>Peterson, R. G. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=.">.</a> Agricultural Field Experiments: Design and Analysis. , (1994).</li><li>Follett, R. F. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Innovative+15N+microplot+research+techniques+to+study+nitrogen+use+efficiency+under+different+ecosystems.">Innovative 15N microplot research techniques to study nitrogen use efficiency under different ecosystems.</a> Communications in Soil Science and Plant Analysis. 32 (7/8), 951-979 (2001).</li><li>Russelle, M. P., Deibert, E. J., Hauck, R. D., Stevanovic, M., Olson, R. A. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Effects+of+water+and+nitrogen+management+on+yield+and+15N-depleted+fertilizer+use+efficiency+of+irrigated+corn.">Effects of water and nitrogen management on yield and 15N-depleted fertilizer use efficiency of irrigated corn.</a> Soil Science Society of America Journal. 45 (3), 553-558 (1981).</li><li>Schindler, F. V., Knighton, R. E. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of+Fertilizer+Nitrogen+Applied+to+Corn+as+Estimated+by+the+Isotopic+and+Difference+Methods.">Fate of Fertilizer Nitrogen Applied to Corn as Estimated by the Isotopic and Difference Methods.</a> Soil Science Society of America Journal. 63, 1734 (1999).</li><li>Stevens, W. B., Hoeft, R. G., Mulvaney, R. L. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of+Nitrogen-15+in+a+Long-Term+Nitrogen+Rate+Study.">Fate of Nitrogen-15 in a Long-Term Nitrogen Rate Study.</a> Agronomy Journal. 97 (4), 1037 (2005).</li><li>Recous, S., Fresneau, C., Faurie, G., Mary, B. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=The+fate+of+labelled+15N+urea+and+ammonium+nitrate+applied+to+a+winter+wheat+crop.">The fate of labelled 15N urea and ammonium nitrate applied to a winter wheat crop.</a> Plant and Soil. 112 (2), 205-214 (1988).</li><li>Abendroth, L. J., Elmore, R. W., Boyer, M. J., Marlay, S. K. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=.">.</a> Corn Growth and Development. , (2011).</li><li>Gomez, K. A., Gomez, A. A. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=.">.</a> Statistical Procedures for Agricultural Research. , (1984).</li><li>Khan, S. A., Mulvaney, R. L., Brooks, P. D. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Diffusion+Methods+for+Automated+Nitrogen-15+Analysis+using+Acidified+Disks.">Diffusion Methods for Automated Nitrogen-15 Analysis using Acidified Disks.</a> Soil Science Society of America Journal. 62 (2), 406 (1998).</li><li>Horneck, D. A., Miller, R. O. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Determination+of+Total+Nitrogen+in+Plant+Tissue.">Determination of Total Nitrogen in Plant Tissue.</a> Handbook of Reference Methods for Plant Analysis. , 75-84 (1998).</li><li>. Carbon (13C) and Nitrogen (15N) Analysis of Solids by EA-IRMS Available from: <a target="_blank" href="https://stableisotopefacility.ucdavis.edu/13cand15n.html">https://stableisotopefacility.ucdavis.edu/13cand15n.html</a> (2019)</li><li>Stevens, W. B., Hoeft, R. G., Mulvaney, R. L. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of+Nitrogen-15+in+a+Long-Term+Nitrogen+Rate+Study:+II.+Nitrogen+Uptake+Efficiency.">Fate of Nitrogen-15 in a Long-Term Nitrogen Rate Study: II. Nitrogen Uptake Efficiency.</a> Agronomy Journal. 97 (4), 1046 (2005).</li><li>. Fertilizing Corn in Minnesota Available from: <a target="_blank" href="https://extension.umn.edu/crop-specific-needs/fertilizing-corn-minnesota">https://extension.umn.edu/crop-specific-needs/fertilizing-corn-minnesota</a> (2018)</li><li>Blake, G. R., Hartge, K. H. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Bulk+Density.">Bulk Density.</a> Methods of Soil Analysis: Part 1 Physical and Mineralogical Methods. , 363-375 (1986).</li><li>Jokela, W. E., Randall, G. W. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of+Fertilizer+Nitrogen+as+Affected+by+Time+and+Rate+of+Application+on+Corn.">Fate of Fertilizer Nitrogen as Affected by Time and Rate of Application on Corn.</a> Soil Science Society of America Journal. 61 (6), 1695 (2010).</li><li>Hart, S. C., Stark, J. M., Davidson, E. A., Firestone, M. K. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Nitrogen+Mineralization,+Immobilization,+and+Nitrification.">Nitrogen Mineralization, Immobilization, and Nitrification.</a> Methods of Soil Analysis, Part 2. Microbiological and Biochemical Properties. (5), 985-1018 (1994).</li><li>Olson, R. V. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of+tagged+nitrogen+fertilizer+applied+to+irrigated+corn.">Fate of tagged nitrogen fertilizer applied to irrigated corn.</a> Soil Science Society of America Journal. 44 (3), 514-517 (1980).</li><li>Follett, R. F., Porter, L. K., Halvorson, A. D. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Border+Effects+on+Nitrogen-15+Fertilized+Winter+Wheat+Microplots+Grown+in+the+Great+Plains.">Border Effects on Nitrogen-15 Fertilized Winter Wheat Microplots Grown in the Great Plains.</a> Agronomy Journal. 83 (3), 608-612 (1991).</li><li>Balabane, M., Balesdent, J. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Input+of+fertilizer-derived+labelled+n+to+soil+organic+matter+during+a+growing+season+of+maize+in+the+field.">Input of fertilizer-derived labelled n to soil organic matter during a growing season of maize in the field.</a> Soil Biology and Biochemistry. 24 (2), 89-96 (1992).</li><li>Recous, S., Machet, J. M., Mary, B. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=The+partitioning+of+fertilizer-N+between+soil+and+crop:+Comparison+of+ammonium+and+nitrate+applications.">The partitioning of fertilizer-N between soil and crop: Comparison of ammonium and nitrate applications.</a> Plant and Soil. 144 (1), 101-111 (1992).</li><li>Bigeriego, M., Hauck, R. D., Olson, R. A. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Uptake,+Translocation+and+Utilization+of+15N-Depleted+Fertilizer+in+Irrigated+Corn.">Uptake, Translocation and Utilization of 15N-Depleted Fertilizer in Irrigated Corn.</a> Soil Science Society of America Journal. 43 (3), 528 (1979).</li><li>Glendining, M. J., Poulton, P. R., Powlson, D. S., Jenkinson, D. S. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Fate+of15N-labelled+fertilizer+applied+to+spring+barley+grown+on+soils+of+contrasting+nutrient+status.">Fate of15N-labelled fertilizer applied to spring barley grown on soils of contrasting nutrient status.</a> Plant and Soil. 195 (1), 83-98 (1997).</li><li>Khanif, Y. M., Cleemput, O., Baert, L. <a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?db=PubMed&cmd=Search&doptcmdl=Citation&defaultField=Title+Word&term=Field+study+of+the+fate+of+labelled+fertilizer+nitrate+applied+to+barley+and+maize+in+sandy+soils.">Field study of the fate of labelled fertilizer nitrate applied to barley and maize in sandy soils.</a> Fertilizer Research. 5 (3), 289-294 (1984).</li></ol>

Stable isotope research is a useful tool for tracking and quantifying FDN through the soil-crop system. However, there are three main assumptions associated with N tracer studies that if violated may invalidate conclusions drawn from using this methodology. They are 1) the tracer is uniformly distributed throughout the system, 2) processes under the study occur at the same rates, and 3) N leaving the 15N enriched pool does not return3. Because this study is interested in the distributio...

Fertilizer nitrogen (N) use is essential in agriculture to meet the food, fiber, feed, and fuel demands of a growing global population, but N losses from agricultural fields can negatively impact environmental quality. Because N undergoes many transformations in the soil-crop system, a better understanding of N cycling, crop utilization, and the overall fate of fertilizer N are necessary to improve management practices that promote N use efficiency and minimize environmental losses. Traditional N fertilizer studies primarily focus on the effect of a treatment on end-of-season measurements such as crop yield, crop N uptake relative to the N rate applied (apparent fertilizer use efficiency), and residual soil N. While these studies quantify the overall system N inputs, outputs, and efficiencies, they cannot identify nor quantify N in the soil-crop system derived from fertilizer sources or the soil. A different approach using stable isotopes must be used to track and quantify the fate of fertilizer derived N (FDN) in the soil-crop system.
Nitrogen has two stable isotopes, 14N and 15N, that occur in nature at a relatively constant ratio of 272:1 for 14N/15N1 (concentration of 0.366 atom % 15N or 3600 ppm 15N2,3). The addition of 15N enriched fertilizer increases the total 15N content of the soil system. As 15N enriched fertilizer mixes with unenriched soil N, the measured change of 14N/15N ratio allows researchers to trace FDN in the soil profile and into the crop3,4. A mass balance can be calculated by measuring the total amount of 15N tracer in the system and each of its parts2. Because 15N enriched fertilizers are significantly more expensive than conventional fertilizers, 15N enriched microplots are often embedded within the treatment plots. The purpose of this methods paper is to describe a small-plot research&#160;design utilizing microplots for multiple in-season soil and plant sampling events for corn (Zea mays L.) and to present protocols for preparing plant and soil samples for total 15N analysis. These results can then be used to estimate N fertilizer use efficiency and create a partial N budget accounting for FDN in the bulk soil and the crop.

<table border="1" fo:keep-together.within-page="1" fo:keep-with-next.within-page="always">
	<tbody>
		<tr>
			<td>20 mL scintillation vial</td>
			<td>ANY; Fisher Scientific is one example</td>
			<td>0334172C</td>
			<td></td>
		</tr>
		<tr>
			<td>250 mL borosilicate glass bottle</td>
			<td>QORPAK</td>
			<td>264047</td>
			<td></td>
		</tr>
		<tr>
			<td>48-well plate</td>
			<td>EA Consumables</td>
			<td>E2063</td>
			<td></td>
		</tr>
		<tr>
			<td>96-well plate</td>
			<td>EA Consumables</td>
			<td>E2079</td>
			<td></td>
		</tr>
		<tr>
			<td>Cloth parts bag (30x50 cm)</td>
			<td>ANY</td>
			<td>NA</td>
			<td>For corn ears</td>
		</tr>
		<tr>
			<td>CO2 Backpack Sprayer</td>
			<td>ANY; Bellspray Inc is one example</td>
			<td>Model T</td>
			<td></td>
		</tr>
		<tr>
			<td>Coin envelop (6.4x10.8 cm)</td>
			<td>ANY; ULINE is one example</td>
			<td>S-6285</td>
			<td>For 2-mm ground plant samples</td>
		</tr>
		<tr>
			<td>Corn chipper</td>
			<td>ANY; DR Chipper Shredder is one example</td>
			<td>SKU:CS23030BMN0</td>
			<td>For chipping corn biomass</td>
		</tr>
		<tr>
			<td>Corn seed</td>
			<td>ANY</td>
			<td>NA</td>
			<td>Hybrid appropriate to the region</td>
		</tr>
		<tr>
			<td>Disposable shoe cover</td>
			<td>ANY; Boardwalk is one example</td>
			<td>BWK00031L</td>
			<td></td>
		</tr>
		<tr>
			<td>Ethanol 200 Proof</td>
			<td>ANY; Decon Laboratories Inc. is one example</td>
			<td>2701TP</td>
			<td></td>
		</tr>
		<tr>
			<td>Fabric bags with drawstring (90x60 cm)</td>
			<td>ANY</td>
			<td>NA</td>
			<td>For plant sample collection</td>
		</tr>
		<tr>
			<td>Fertilizer Urea (46-0-0)</td>
			<td>ANY</td>
			<td>NA</td>
			<td>~0.366 atom % 15N</td>
		</tr>
		<tr>
			<td>Hand rake</td>
			<td>ANY; Fastenal Company is one example</td>
			<td>5098-63-107</td>
			<td></td>
		</tr>
		<tr>
			<td>Hand sickle</td>
			<td>ANY; Home Depot is one example</td>
			<td>NJP150</td>
			<td>For plant sample collection</td>
		</tr>
		<tr>
			<td>Hand-held soil probe</td>
			<td>ANY; AMS is one example</td>
			<td>401.01</td>
			<td></td>
		</tr>
		<tr>
			<td>Hydraulic soil probe</td>
			<td>ANY; Giddings is one example</td>
			<td>GSPS</td>
			<td></td>
		</tr>
		<tr>
			<td>Hydrochloric acid, 12N</td>
			<td>Ricca Chemical</td>
			<td>R37800001A</td>
			<td></td>
		</tr>
		<tr>
			<td>Jar mill</td>
			<td>ANY; Cole-Parmer is one example</td>
			<td>SI-04172-50</td>
			<td></td>
		</tr>
		<tr>
			<td>Laboratory Mill</td>
			<td>Perten</td>
			<td>3610</td>
			<td>For grinding grain</td>
		</tr>
		<tr>
			<td>Microbalance accurate to four decimal places</td>
			<td>ANY; Mettler Toledo is one example</td>
			<td>XPR2</td>
			<td></td>
		</tr>
		<tr>
			<td>N95 Particulate Filtering Facepiece Respirator</td>
			<td>ANY, ULINE is one example</td>
			<td>S-9632</td>
			<td></td>
		</tr>
		<tr>
			<td>Neoprene or butyl rubber gloves</td>
			<td>ANY</td>
			<td>NA</td>
			<td>For working in HCl acid bath</td>
		</tr>
		<tr>
			<td>Paper hardware bags (13.3x8.7x27.8 cm)</td>
			<td>ANY; ULINE is one example</td>
			<td>S-8530</td>
			<td>For soil samples and corn grain</td>
		</tr>
		<tr>
			<td>Plant grinder</td>
			<td>ANY; Thomas Wiley Model 4 Mill is one example</td>
			<td>1188Y47-TS</td>
			<td>For grinding chipped corn biomass to 2-mm particles</td>
		</tr>
		<tr>
			<td>Plastic tags</td>
			<td>ULINE</td>
			<td>S-5544Y-PW</td>
			<td>For labeling fabric bags and microplot stalk bundles</td>
		</tr>
		<tr>
			<td>Sodium hydroxide pellets, ACS</td>
			<td>Spectrum Chemical</td>
			<td>SPCM-S1295-07</td>
			<td></td>
		</tr>
		<tr>
			<td>Soil grinder</td>
			<td>ANY; AGVISE stainless steel grinder with motor is one example</td>
			<td>NA</td>
			<td>For grinding soil to pass through a 2-mm sieve</td>
		</tr>
		<tr>
			<td>Tin capsule 5x9 mm</td>
			<td>Costech Analytical Technologies Inc.</td>
			<td>041061</td>
			<td></td>
		</tr>
		<tr>
			<td>Tin capsule 9x10 mm</td>
			<td>Costech Analytical Technologies Inc.</td>
			<td>041073</td>
			<td></td>
		</tr>
		<tr>
			<td>Urea (46-0-0)</td>
			<td>MilliporeSigma</td>
			<td>490970</td>
			<td>10 atom % 15N</td>
		</tr>
	</tbody>
</table>

microplot design and plant and soil sample preparation for 15nitrogen analysis

Many&#160;nitrogen fertilizer studies evaluate the overall effect of a treatment on end-of-season measurements such as grain yield or cumulative N losses. A stable isotope approach is necessary to follow and quantify the fate of fertilizer derived N (FDN) through the soil-crop system. The purpose of this paper is to describe a small-plot research&#160;design utilizing non-confined 15N enriched microplots for multiple soil and plant sampling events over two growing seasons and provide sample collection, handling, and processing protocols for total 15N analysis. The methods were demonstrated using a replicated study from south-central Minnesota planted to corn (Zea mays L.). Each treatment consisted of six corn rows (76 cm row-spacing) 15.2 m long with a microplot (2.4 m by 3.8 m) embedded at one end. Fertilizer-grade urea was applied at 135 kg N&#8729;ha-1 at planting, while the microplot received urea enriched to 5 atom % 15N. Soil and plant samples were taken several times throughout the growing season, taking care to minimize cross-contamination by using separate tools and physically separating unenriched and enriched samples during all procedures. Soil and plant samples were dried, ground to pass through a 2 mm screen, and then ground to a flour-like consistency using a roller jar mill. Tracer studies require additional planning, sample processing time and manual labor, and incur higher costs for 15N enriched materials and sample analysis than traditional N studies. However, using the mass balance approach, tracer studies with multiple in-season sampling events allow the researcher to estimate FDN distribution through the soil-crop system and estimate unaccounted-for FDN from the system.

The results presented in this paper come from a field site established in 2015 at the University of Minnesota Southern Outreach and Research Center located near Waseca, MN. The site was managed as a corn-soybean [Glycine max (L.) Merr] rotation prior to 2015 but was managed as a corn-corn rotation during the 2015 and 2016 growing seasons. The soil was a Nicollet clay loam (fine-loamy, mixed, superactive, mesic Aquic Hapludolls)-Webster clay loam (fine-loamy, mixed, superactive, m...

Watch this Scientific Journal Video about Microplot Design and Plant and Soil Sample Preparation for 15Nitrogen Analysis at JoVE.com

Microplot Design and Plant and Soil Sample Preparation for 15Nitrogen Analysis

A microplot design for 15N tracer research is described to accommodate multiple in-season plant and soil sampling events. Soil and plant sample collection and processing procedures, including grinding and weighing protocols, for 15N analysis are put forth.

Microplot Design and Plant and Soil Sample Preparation for 15Nitrogen Analysis

Many&#160;nitrogen fertilizer studies evaluate the overall effect of a treatment on end-of-season measurements such as grain yield or cumulative N losses. ...

This methodology can help researchers quantify the impacts of fertilizer drive nitrogen on the soil crop system and answer questions about nitrogen use efficiency. The main advantage of this technique is that it allows for multiple in seasons soil and plant sampling events over two consecutive growing seasons. This methodology could help us better understand the nitrogen cycle processes of mineralization and mobilization to improve nitrogen fertilizer management guidelines.To set up a field plot, plant six cornrows with 76 centimeters of spacing with a final 15.2 by 4.6 meter plot dimension. Establish 1.5 meter border areas from each end of the lengthwise dimension and an additional 1.5 meter long border area adjoining the sampling and harvest areas. Designate rows two and three as the in season plant and soil sampling area and rows four and five as the harvest area for corn grain yield.Establish a 2.4 by 3.8 meter micro plot area centered on the width dimension for collection of all the nitrogen enriched plant and soil samples, leaving 38 meters of unsampled border on the length and width dimensions to minimize any edge effects. Then delineate the treatment plot and micro plot corners with different colored flags. Wear shoe coverings when accessing the micro plots and minimize micro plot foot traffic to prevent contamination of the unenriched sampling areas, removing the foot covers when exiting the micro plot area.To apply the Nitrogen-15 enriched fertilizer, dilute 10 atom percent Nitrogen-15 enriched urea in conventional urea to five atom percent nitrogen enriched urea and dissolve the urea in two liters of deionized water to ensure uniform enrichment of the urea fertilizer. Use a calibrated backpack carbon dioxide sprayer to evenly apply the Nitrogen-15 enriched urea solution to the micro plots. Then incorporate urea containing fertilizers with light tillage, hand rakes or 64 centimeters of irrigation within 24 hours of application to minimize the volatilization loss potential.At each sampling stage, collect a six above ground, Nitrogen-15 unenriched corn plant composite sample from within the sampling area and a six above ground corn plant composite sample from the Nitrogen-15 enriched micro plot. Chop VH and R1 above ground biomasses and place the chopped biomass in labeled bags or drying and a forced air oven at 60 degrees Celsius until constant mass. Record the biomass dry weight and thoroughly mix and grind 100 to 200 grams of dried plant material until it can pass through a two millimeter sieve.Then thoroughly mix the ground material and store the sub sample in a labeled coin envelope for further processing. For soil sample processing, within eight days of fertilizer application, use a hand probe to collect a four core 1.8 centimeter diameter composite soil sample from the unenriched sampling area at VH and R1 concurrent with the plant sampling and use a separate hand probe to collect a 15 core 1.8 centimeter diameter composite soil sample from the micro plot. Homogenize each composite soil sample in a bucket and place the samples in pre labeled paper bags.Then drY the soil samples at 35 degrees Celsius in a forced air oven until constant mass, before grinding each sample until it can pass through a two millimeter sieve. For sample processing in the laboratory dry the ground plan samples overnight in the 60 degrees Celsius oven, before individually grinding the dried plant and soil samples in roller jars at four times g for six to 24 hours until the samples obtain a fine flour like consistency. Then transfer the finely ground material into clean labeled 20 milliliters silylation vials.To determine the total and Nitrogen-15 concentration in each sample, wearing nitrile gloves, first use laboratory wipes and ethanol to clean the micro scale, work surfaces, spatula and forceps. Place the clean utensils on a lab wipe on the lab bench and use forceps to gently flare out the opening of the sample capsule. Oven and release the modified capsule one to two millimeters above the micro scale weigh pan and tear the capsule.Use forceps to return the capsule to the clean work surface and use the spatula to carefully add the required mass of finely ground sample material to the capsule. Use the forceps to slowly crimp the top third of the loaded capsule and fold over to seal. Continue folding and compressing the capsule, taking care not to puncture or tear the tin until a spherical shape has been obtained.Use the forceps to drop the wrapped capsule several times from a one centimeter height onto a clean dark surface to check for leaks. If no dust appears, weigh the sample as just demonstrated and place the capsule in one well of a 96 well plate, recording the well placement. Between each sample encapsulation, clean each of the utensils and surfaces with ethanol and laboratory wipes, paying special attention to the spatula and forceps edges.In this representative analysis, the fertilizer-derived nitrogen concentration in the above ground corn biomass sample was greatest earlier in the growing season and decreased with each successive sampling period. The soil-derived nitrogen however, was consistently the greatest fraction of above ground biomass nitrogen, illustrating the importance of the soil nitrogen supply for optimal corn growth. At physiological maturity in the first year, approximately 27%of the above ground biomass nitrogen was fertilizer-derived with similar proportions observed in the grain, stover and cob fractions.At physiological maturity in the second year, only 2%of first year fertilizer-derived nitrogen was recovered in the above ground biomass. With approximately 1.6 kilograms per hectare of first year fertilizer derived nitrogen exported in the grain. Within eight days of fertilizer application, the majority of the fertilizer derived nitrogen was in the top 15 centimeters of the soil profile as expected.However approximately 22 kilograms of nitrogen per hectare had already moved into the deeper depths, while four to 10%of the fertilizer-derived nitrogen was unaccounted for. Indeed, by the end of the first and second years, less than 50%of the fertilizer-derived nitrogen was accounted for within the soil corn system, while the remainder was either lost to the environment or leached below the 90 centimeter soil sample depth. When attempting this procedure, extreme care should be taken to avoid cross contamination which can invalidate the results.Inorganic and organic fractions of the soil may be further analyzed to improve our understanding of nitrogen cycling dynamics. Plant samples analyzed by plant parts may be used to inform our understanding of nitrogen uptake and translocation over time.

microplot-design-plant-soil-sample-preparation-for-15nitrogen

Research

JoVE Journal

Environment

Design and Operation of a Continuous 13C and 15N Labeling Chamber for Uniform or Differential, Metabolic and Structural, Plant Isotope Labeling

Tracing rare stable isotopes from plant material through the ecosystem provides the most sensitive information about ecosystem processes; from CO2 fluxes and soil organic matter formation to small-scale stable-isotope biomarker probing. Coupling multiple stable isotopes such as 13C with 15N, 18O or&#160;2H has the potential to reveal even more information about complex stoichiometric relationships during biogeochemical transformations. Isotope labeled plant material has been used in various studies of litter decomposition and soil organic matter formation1-4. From these and other studies, however, it has become apparent that structural components of plant material behave differently than metabolic components (i.e. leachable low molecular weight compounds) in terms of microbial utilization and long-term carbon storage5-7. The ability to study structural and metabolic components separately provides a powerful new tool for advancing the forefront of ecosystem biogeochemical studies. Here we describe a method for producing 13C and 15N labeled plant material that is either uniformly labeled throughout the plant or differentially labeled in structural and metabolic plant components.
Here, we present the construction and operation of a continuous 13C and 15N labeling chamber that can be modified to meet various research needs. Uniformly labeled plant material is produced by continuous labeling from seedling to harvest, while differential labeling is achieved by removing the growing plants from the chamber weeks prior to harvest. Representative results from growing Andropogon gerardii Kaw demonstrate the system&#39;s ability to efficiently label plant material at the targeted levels. Through this method we have produced plant material with a 4.4 atom%13C and 6.7 atom%15N uniform plant label, or material that is differentially labeled by up to 1.29 atom%13C and 0.56 atom%15N in its metabolic and structural components (hot water extractable and hot water residual components, respectively). Challenges lie in maintaining proper temperature, humidity, CO2 concentration,&#160;and light levels in an airtight 13C-CO2 atmosphere for successful plant production. This chamber description represents a useful research tool to effectively produce uniformly or differentially multi-isotope labeled plant material for use in experiments on ecosystem biogeochemical cycling.

Design and Operation of a Continuous 13C and 15N Labeling Chamber for Uniform or Differential, Metabolic and Structural, Plant Isotope Labeling

This method explains how to build and operate a continuous 13C and 15N isotope labeling chamber for uniform or differential plant tissue labeling. Representative results from metabolic and structural labeling of Andropogon gerardii are discussed.

Tracing rare stable isotopes from plant material through the ecosystem provides the most sensitive information about ecosystem processes; from CO2 fluxes ...

Design and Construction of an Urban Runoff Research Facility

As the urban population increases, so does the area of irrigated urban landscape. Summer water use in urban areas can be 2-3x winter base line water use due to increased demand for landscape irrigation. Improper irrigation practices and large rainfall events can result in runoff from urban landscapes which has potential to carry nutrients and sediments into local streams and lakes where they may contribute to eutrophication. A 1,000 m2 facility was constructed which consists of 24 individual 33.6 m2 field plots, each equipped for measuring total runoff volumes with time and collection of runoff subsamples at selected intervals for quantification of chemical constituents in the runoff water from simulated urban landscapes. Runoff volumes from the first and second trials had coefficient of variability (CV) values of 38.2 and 28.7%, respectively. CV values for runoff pH, EC, and Na concentration for both trials were all under 10%. Concentrations of DOC, TDN, DON, PO4-P, K+, Mg2+, and Ca2+ had CV values less than 50% in both trials. Overall, the results of testing performed after sod installation at the facility indicated good uniformity between plots for runoff volumes and chemical constituents. The large plot size is sufficient to include much of the natural variability and therefore provides better simulation of urban landscape ecosystems.

This paper describes the design, construction, and function of a 1,000 m2 facility containing 24 individual 33.6 m2 field plots equipped for measuring total runoff volumes with time and collection of runoff subsamples at selected intervals for quantification of chemical constituents in the runoff water from simulated home lawns.

As the urban population increases, so does the area of irrigated urban landscape. Summer water use in urban areas can be 2-3x winter base line water use ...

Experimental Protocol for Manipulating Plant-induced Soil Heterogeneity

Coexistence theory has often treated environmental heterogeneity as being independent of the community composition; however biotic feedbacks such as plant-soil feedbacks (PSF) have large effects on plant performance, and create environmental heterogeneity that depends on the community composition. Understanding the importance of PSF for plant community assembly necessitates understanding of the role of heterogeneity in PSF, in addition to mean PSF effects. Here, we describe a protocol for manipulating plant-induced soil heterogeneity. Two example experiments are presented: (1) a field experiment with a 6-patch grid of soils to measure plant population responses and (2) a greenhouse experiment with 2-patch soils to measure individual plant responses. Soils can be collected from the zone of root influence (soils from the rhizosphere and directly adjacent to the rhizosphere) of plants in the field from conspecific and heterospecific plant species. Replicate collections are used to avoid pseudoreplicating soil samples. These soils are then placed into separate patches for heterogeneous treatments or mixed for a homogenized treatment. Care should be taken to ensure that heterogeneous and homogenized treatments experience the same degree of soil disturbance. Plants can then be placed in these soil treatments to determine the effect of plant-induced soil heterogeneity on plant performance. We demonstrate that plant-induced heterogeneity results in different outcomes than predicted by traditional coexistence models, perhaps because of the dynamic nature of these feedbacks. Theory that incorporates environmental heterogeneity influenced by the assembling community and additional empirical work is needed to determine when heterogeneity intrinsic to the assembling community will result in different assembly outcomes compared with heterogeneity extrinsic to the community composition.

Understanding the role of environmental heterogeneity in species coexistence has typically focused on types of heterogeneity that are extrinsic to the community&#8217;s species composition. We provide novel detailed methods for creating soil heterogeneity treatments using soils subject to plant-soil feedback conditioning, or heterogeneity intrinsic to the community composition.

Coexistence theory has often treated environmental heterogeneity as being independent of the community composition; however biotic feedbacks such as ...

A Gusseted Thermogradient Table to Control Soil Temperatures for Evaluating Plant Growth and Monitoring Soil Processes

Thermogradient tables were first developed in the 1950s primarily to test seed germination over a range of temperatures simultaneously without using a series of incubators. A temperature gradient is passively established across the surface of the table between the heated and cooled ends and is lost quickly at distances above the surface. Since temperature is only controlled on the table surface, experiments are restricted to shallow containers, such as Petri dishes, placed on the table. Welding continuous aluminum vertical strips or gussets perpendicular to the surface of a table enables temperature control in depth via convective heat flow. Soil in the channels between gussets was maintained across a gradient of temperatures allowing a greater diversity of experimentation. The gusseted design was evaluated by germinating oat, lettuce, tomato, and melon seeds. Soil temperatures were monitored using individual, battery-powered dataloggers positioned across the table. LED lights installed in the lids or along the sides of the gradient table create a controlled temperature chamber where seedlings can be grown over a range of temperatures. The gusseted design enabled accurate determination of optimum temperatures for fastest germination rate and the highest percentage germination for each species. Germination information from gradient table experiments can help predict seed germination and seedling growth under the adverse soil conditions often encountered during field crop production. Temperature effects on seed germination, seedling growth, and soil ecology can be tested under controlled conditions in a laboratory using a gusseted thermogradient table.

Traditional thermogradient tables create a range of temperatures across the surface. Welding gussets perpendicular to the surface of a thermogradient table will control temperature in depth increasing possible research applications.

Thermogradient tables were first developed in the 1950s primarily to test seed germination over a range of temperatures simultaneously without using a ...

Protocol for Microplastics Sampling on the Sea Surface and Sample Analysis

Microplastic pollution in the marine environment is a scientific topic that has received increasing attention over the last decade. The majority of scientific publications address microplastic pollution of the sea surface. The protocol below describes the methodology for sampling, sample preparation, separation and chemical identification of microplastic particles. A manta net fixed on an &#187;A frame&#171; attached to the side of the vessel was used for sampling. Microplastic particles caught in the cod end of the net were separated from samples by visual identification and use of stereomicroscopes. Particles were analyzed for their size using an image analysis program and for their chemical structure using ATR-FTIR and micro FTIR spectroscopy. The described protocol is in line with recommendations for microplastics monitoring published by the Marine Strategy Framework Directive (MSFD) Technical Subgroup on Marine Litter. This written protocol with video guide will support the work of researchers that deal with microplastics monitoring all over the world.

The protocol below describes the methodology for: microplastics sampling on the sea surface, separation of microplastic and chemical identification of particles. This protocol is in line with the recommendations for microplastics monitoring published by the MSFD Technical Subgroup on Marine Litter.

Microplastic pollution in the marine environment is a scientific topic that has received increasing attention over the last decade. The majority of ...

Nanopore DNA Sequencing for Metagenomic Soil Analysis

This article describes the steps for construction of a DNA library from soil, preparation and use of the nanopore flow cell, and analysis of the DNA sequences identified using computer software. Nanopore DNA sequencing is a flexible technique that allows for rapid microbial genome sequencing to identify bacterial and viral species, to characterize bacterial strains, and to detect genetic mutations that confer resistance to antibiotics. The advantages of nanopore sequencing (NS) for life sciences include its low complexity, reduced cost, and rapid real-time sequencing of purified genomic DNA, PCR amplicons, cDNA samples, or RNA. NS is an example of "strand sequencing" which involves sequencing DNA by guiding a single stranded DNA molecule through a nanopore that is inserted into a synthetic polymer membrane. The membrane has an electrical current applied across it, so as the individual bases pass through the nanopore the electrical current is disrupted to varying degrees by the four nucleotide bases. The identification of each nucleotide occurs by detecting the characteristic modulation of the electrical current by the different bases as they pass through the nanopore. The NS system consists of a handheld, USB powered portable device and a disposable flow cell that contains a nanopore array. The portable device plugs into a standard laptop computer that reads and records the DNA sequence using computer software.

Nanopore technology for sequencing biomolecules has wide applications in the life sciences, including identification of pathogens, food safety monitoring, genomic analysis, metagenomic environmental monitoring, and characterization of bacterial antibiotic resistance. In this article, the procedure for metagenomic soil DNA sequencing for species identification using the nanopore sequencing technology is demonstrated.

This article describes the steps for construction of a DNA library from soil, preparation and use of the nanopore flow cell, and analysis of the DNA ...

Isolation and Analysis of Microbial Communities in Soil, Rhizosphere, and Roots in Perennial Grass Experiments

Plant and soil microbiome studies are becoming increasingly important for understanding the roles microorganisms play in agricultural productivity. The purpose of this manuscript is to provide detail on how to rapidly sample soil, rhizosphere, and endosphere of replicated field trials and analyze changes that may occur in the microbial communities due to sample type, treatment, and plant genotype. The experiment used to demonstrate these methods consists of replicated field plots containing two, pure, warm-season grasses (Panicum virgatum and Andropogon gerardii) and a low-diversity grass mixture (A. gerardii, Sorghastrum nutans, and Bouteloua curtipendula). Briefly, plants are excavated, a variety of roots are cut and placed in phosphate buffer, and then shaken to collect the rhizosphere. Roots are brought to the laboratory on ice and surface sterilized with bleach and ethanol (EtOH). The rhizosphere is filtered and concentrated by centrifugation. Excavated soil from around the root ball is placed into plastic bags and brought to the lab where a small amount of soil is taken for DNA extractions. DNA is extracted from roots, soil, and rhizosphere and then amplified with primers for the V4 region of the 16S rRNA gene. Amplicons are sequenced, then analyzed with open access bioinformatics tools. These methods allow researchers to test how the microbial community diversity and composition varies due to sample type, treatment, and plant genotype. Using these methods along with statistical models, the representative results demonstrate there are significant differences in microbial communities of roots, rhizosphere, and soil. Methods presented here provide a complete set of steps for how to collect field samples, isolate, extract, quantify, amplify, and sequence DNA, and analyze microbial community diversity and composition in replicated field trials.

Excavation of plant roots from the field as well as processing of samples into endosphere, rhizosphere, and soil are described in detail, including DNA extraction and data analysis methods. This paper is designed to enable other laboratories to use these techniques for the study of soil, endosphere, and rhizosphere microbiomes.

Plant and soil microbiome studies are becoming increasingly important for understanding the roles microorganisms play in agricultural productivity. The ...

High-throughput Siderophore Screening from Environmental Samples: Plant Tissues, Bulk Soils, and Rhizosphere Soils

Siderophores (low-molecular weight metal chelating compounds) are important in various ecological phenomenon ranging from iron (Fe) biogeochemical cycling in soils, to pathogen competition, plant growth promotion, and cross-kingdom signaling. Furthermore, siderophores are also of commercial interest in bioleaching and bioweathering of metal-bearing minerals and ores. A rapid, cost effective, and robust means of quantitatively assessing siderophore production in complex samples is key to identifying important aspects of the ecological ramifications of siderophore activity, including, novel siderophore producing microbes. The method presented here was developed to assess siderophore activity of in-tact microbiome communities, in environmental samples, such as soil or plant tissues. The samples were homogenized and diluted in a modified M9 medium (without Fe), and enrichment cultures were incubated for 3 days. Siderophore production was assessed in samples at 24, 48, and 72 hours (h) using a novel 96-well microplate CAS (Chrome azurol sulphonate)-Fe agar assay, an adaptation of the traditionally tedious and time-consuming colorimetric method of assessing siderophore activity, performed on individual cultivated microbial isolates. We applied our method to 4 different genotypes/Lines of wheat (Triticum aestivum L.), including Lewjain, Madsen, and PI561725, and PI561727 commonly grown in the inland Pacific Northwest. Siderophore production was clearly impacted by the genotype of wheat, and in the specific types of plant tissues observed. We successfully used our method to rapidly screen for the influence of plant genotype on siderophore production, a key function in terrestrial and aquatic ecosystems. We produced many technical replicates, yielding very reliable statistical differences in soils and within plant tissues. Importantly, the results show the proposed method can be used to rapidly examine siderophore production in complex samples with a high degree of reliability, in a manner that allows communities to be preserved for later work to identify taxa and functional genes.

We present a protocol for rapid screening of environmental samples for siderophore potential contributing to micronutrient bioavailability and turnover in terrestrial systems.

Siderophores (low-molecular weight metal chelating compounds) are important in various ecological phenomenon ranging from iron (Fe) biogeochemical cycling ...

Sample Preparation Method of Scanning and Transmission Electron Microscope for the Appendages of Woodboring Beetle

This report described sample preparation methods that scanning and transmission electron microscope observations, demonstrated by preparing appendages of the woodboring beetle, Chlorophorus caragana Xie &#38; Wang (2012), for both types of electron microscopy. The scanning electron microscopy (SEM) sample preparation protocol was based on sample chemical fixation, dehydration in a series of ethanol baths, drying, and sputter-coating. By adding Tween 20 (Polyoxyethylene sorbitan laurate) to the fixative and the wash solution, the insect body surface of woodboring beetle was washed more cleanly in SEM. This study&#39;s transmission electron microscopy (TEM) sample preparation involved a series of steps including fixation, ethanol dehydration, embedding in resin, positioning using fluorescence microscopy, sectioning, and staining. Fixative with Tween 20 enabled penetrate the insect body wall of woodboring beetle more easily than it would had been without Tween 20, and subsequently better fixed tissues and organs in the body, thus yielded clear transmission electron microscope observations of insect sensilla ultrastructures. The next step of this preparation was determining the positions of insect sensilla in the sample embedded in the resin block by using fluorescence microscopy to increase the precision of target sensilla positioning. This improved slicing accuracy.

In order to observe ultrastructure of insect sensilla, scanning and transmission electron microscopy (SEM and TEM, respectively) sample preparation protocol were presented in the study. Tween 20 was added into the fixative to avoid sample deformation in SEM. Fluorescence microscopy was helpful for improving slicing accuracy in TEM.

This report described sample preparation methods that scanning and transmission electron microscope observations, demonstrated by preparing appendages of ...

Measuring Phosphorus Release in Laboratory Microcosms for Water Quality Assessment

Phosphorus (P) is a critical limiting nutrient in agroecosystems requiring careful management to reduce transport risk to aquatic environments. Routine laboratory measures of P bioavailability are based on chemical extractions performed on dried samples under oxidizing conditions. While useful, these tests are limited with respect to characterizing P release under prolonged water saturation. Labile orthophosphate bound to oxidized iron and other metals can rapidly desorb to solution in reducing environments, increasing P mobilization risk to surface runoff and groundwater. To better quantify P desorption potential and mobility during extended saturation, a laboratory microcosm method was developed based on repeated sampling of porewater and overlying floodwater over time. The method is useful for quantifying P release potential from soils and sediments varying in physicochemical properties and can improve site-specific P mitigation efforts by better characterizing P release risk in hydrologically active areas. Advantages of the method include its ability to simulate in situ dynamics, simplicity, low cost, and flexibility.

Accurate quantification of phosphorus (P) desorption potential in saturated soils and sediments is important for P modeling and transport mitigation efforts. To better account for in situ soil-water redox dynamics and P mobilization under prolonged saturation, a simple approach was developed based on repeated sampling of laboratory microcosms.

Phosphorus (P) is a critical limiting nutrient in agroecosystems requiring careful management to reduce transport risk to aquatic environments. Routine ...