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United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen
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Zeitschriftentitel: | Soil Science Society of America Journal |
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Personen und Körperschaften: | , , , , , , , , , , , , , |
In: | Soil Science Society of America Journal, 83, 2019, 4, S. 1137-1147 |
Format: | E-Article |
Sprache: | Englisch |
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author_facet |
Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. |
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author |
Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. |
spellingShingle |
Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. Soil Science Society of America Journal United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen Soil Science |
author_sort |
clark, jason d. |
spelling |
Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. 0361-5995 1435-0661 Wiley Soil Science http://dx.doi.org/10.2136/sssaj2019.02.0047 <jats:sec><jats:label /><jats:p>Nitrogen provided to crops through mineralization is an important factor in N management guidelines. Understanding of the interactive effects of soil and weather conditions on N mineralization needs to be improved. Relationships between anaerobic potentially mineralizable N (PMN<jats:sub>an</jats:sub>) and soil and weather conditions were evaluated under the contrasting climates of eight US Midwestern states. Soil was sampled (0–30 cm) for PMN<jats:sub>an</jats:sub> analysis before pre‐plant N application (PP<jats:sub>0N</jats:sub>) and at the V5 development stage from the pre‐plant 0 (V5<jats:sub>0N</jats:sub>) and 180 kg N ha<jats:sup>−1</jats:sup> (V5<jats:sub>180N</jats:sub>) rates and incubated for 7, 14, and 28 d. Even distribution of precipitation and warmer temperatures before soil sampling and greater soil organic matter (SOM) increased PMN<jats:sub>an</jats:sub>. Soil properties, including total C, SOM, and total N, had the strongest relationships with PMN<jats:sub>an</jats:sub> (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.40), followed by temperature (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.20) and precipitation (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.18) variables. The strength of the relationships between soil properties and PMN<jats:sub>an</jats:sub> from PP<jats:sub>0N</jats:sub>, V5<jats:sub>0N</jats:sub>, and V5<jats:sub>180N</jats:sub> varied by ≤10%. Including soil and weather in the model greatly increased PMN<jats:sub>an</jats:sub> predictability (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.69), demonstrating the interactive effect of soil and weather on N mineralization at different times during the growing season regardless of N fertilization. Delayed soil sampling (V5<jats:sub>0N</jats:sub>) and sampling after fertilization (V5<jats:sub>180N</jats:sub>) reduced PMN<jats:sub>an</jats:sub> predictability. However, longer PMN<jats:sub>an</jats:sub> incubations improved PMN<jats:sub>an</jats:sub> predictability from both V5 soil samplings closer to the PMN<jats:sub>an</jats:sub> predictability from PP<jats:sub>0N</jats:sub>, indicating the potential of PMN<jats:sub>an</jats:sub> from longer incubations to provide improved estimates of N mineralization when N fertilizer is applied.</jats:p></jats:sec><jats:sec><jats:title>Core Ideas</jats:title><jats:p><jats:list list-type="bullet"> <jats:list-item><jats:p>Relationships between mineralization estimates taken with the PMN<jats:sub>an</jats:sub> test and soil and weather conditions need to be improved.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil sample timing and N fertilization minimally affected PMN<jats:sub>an</jats:sub> predictability by soil and weather parameters.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil properties predict PMN<jats:sub>an</jats:sub> better than weather conditions.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil and weather conditions combined explain up to 69% of the variability of PMN<jats:sub>an</jats:sub>.</jats:p></jats:list-item> <jats:list-item><jats:p>Longer PMN<jats:sub>an</jats:sub> incubations improve the relationship between soil and weather parameters and PMN<jats:sub>an</jats:sub> after N fertilization.</jats:p></jats:list-item> </jats:list></jats:p></jats:sec> United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen Soil Science Society of America Journal |
doi_str_mv |
10.2136/sssaj2019.02.0047 |
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Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft |
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Wiley, 2019 |
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English |
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2019 |
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Wiley |
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ai |
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ai |
series |
Soil Science Society of America Journal |
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49 |
title |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_unstemmed |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_full |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_fullStr |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_full_unstemmed |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_short |
United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_sort |
united states midwest soil and weather conditions influence anaerobic potentially mineralizable nitrogen |
topic |
Soil Science |
url |
http://dx.doi.org/10.2136/sssaj2019.02.0047 |
publishDate |
2019 |
physical |
1137-1147 |
description |
<jats:sec><jats:label /><jats:p>Nitrogen provided to crops through mineralization is an important factor in N management guidelines. Understanding of the interactive effects of soil and weather conditions on N mineralization needs to be improved. Relationships between anaerobic potentially mineralizable N (PMN<jats:sub>an</jats:sub>) and soil and weather conditions were evaluated under the contrasting climates of eight US Midwestern states. Soil was sampled (0–30 cm) for PMN<jats:sub>an</jats:sub> analysis before pre‐plant N application (PP<jats:sub>0N</jats:sub>) and at the V5 development stage from the pre‐plant 0 (V5<jats:sub>0N</jats:sub>) and 180 kg N ha<jats:sup>−1</jats:sup> (V5<jats:sub>180N</jats:sub>) rates and incubated for 7, 14, and 28 d. Even distribution of precipitation and warmer temperatures before soil sampling and greater soil organic matter (SOM) increased PMN<jats:sub>an</jats:sub>. Soil properties, including total C, SOM, and total N, had the strongest relationships with PMN<jats:sub>an</jats:sub> (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.40), followed by temperature (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.20) and precipitation (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.18) variables. The strength of the relationships between soil properties and PMN<jats:sub>an</jats:sub> from PP<jats:sub>0N</jats:sub>, V5<jats:sub>0N</jats:sub>, and V5<jats:sub>180N</jats:sub> varied by ≤10%. Including soil and weather in the model greatly increased PMN<jats:sub>an</jats:sub> predictability (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.69), demonstrating the interactive effect of soil and weather on N mineralization at different times during the growing season regardless of N fertilization. Delayed soil sampling (V5<jats:sub>0N</jats:sub>) and sampling after fertilization (V5<jats:sub>180N</jats:sub>) reduced PMN<jats:sub>an</jats:sub> predictability. However, longer PMN<jats:sub>an</jats:sub> incubations improved PMN<jats:sub>an</jats:sub> predictability from both V5 soil samplings closer to the PMN<jats:sub>an</jats:sub> predictability from PP<jats:sub>0N</jats:sub>, indicating the potential of PMN<jats:sub>an</jats:sub> from longer incubations to provide improved estimates of N mineralization when N fertilizer is applied.</jats:p></jats:sec><jats:sec><jats:title>Core Ideas</jats:title><jats:p><jats:list list-type="bullet">
<jats:list-item><jats:p>Relationships between mineralization estimates taken with the PMN<jats:sub>an</jats:sub> test and soil and weather conditions need to be improved.</jats:p></jats:list-item>
<jats:list-item><jats:p>Soil sample timing and N fertilization minimally affected PMN<jats:sub>an</jats:sub> predictability by soil and weather parameters.</jats:p></jats:list-item>
<jats:list-item><jats:p>Soil properties predict PMN<jats:sub>an</jats:sub> better than weather conditions.</jats:p></jats:list-item>
<jats:list-item><jats:p>Soil and weather conditions combined explain up to 69% of the variability of PMN<jats:sub>an</jats:sub>.</jats:p></jats:list-item>
<jats:list-item><jats:p>Longer PMN<jats:sub>an</jats:sub> incubations improve the relationship between soil and weather parameters and PMN<jats:sub>an</jats:sub> after N fertilization.</jats:p></jats:list-item>
</jats:list></jats:p></jats:sec> |
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author | Clark, Jason D., Veum, Kristen S., Fernández, Fabián G., Camberato, James J., Carter, Paul R., Ferguson, Richard B., Franzen, David W., Kaiser, Daniel E., Kitchen, Newell R., Laboski, Carrie A. M., Nafziger, Emerson D., Rosen, Carl J., Sawyer, John E., Shanahan, John F. |
author_facet | Clark, Jason D., Veum, Kristen S., Fernández, Fabián G., Camberato, James J., Carter, Paul R., Ferguson, Richard B., Franzen, David W., Kaiser, Daniel E., Kitchen, Newell R., Laboski, Carrie A. M., Nafziger, Emerson D., Rosen, Carl J., Sawyer, John E., Shanahan, John F., Clark, Jason D., Veum, Kristen S., Fernández, Fabián G., Camberato, James J., Carter, Paul R., Ferguson, Richard B., Franzen, David W., Kaiser, Daniel E., Kitchen, Newell R., Laboski, Carrie A. M., Nafziger, Emerson D., Rosen, Carl J., Sawyer, John E., Shanahan, John F. |
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description | <jats:sec><jats:label /><jats:p>Nitrogen provided to crops through mineralization is an important factor in N management guidelines. Understanding of the interactive effects of soil and weather conditions on N mineralization needs to be improved. Relationships between anaerobic potentially mineralizable N (PMN<jats:sub>an</jats:sub>) and soil and weather conditions were evaluated under the contrasting climates of eight US Midwestern states. Soil was sampled (0–30 cm) for PMN<jats:sub>an</jats:sub> analysis before pre‐plant N application (PP<jats:sub>0N</jats:sub>) and at the V5 development stage from the pre‐plant 0 (V5<jats:sub>0N</jats:sub>) and 180 kg N ha<jats:sup>−1</jats:sup> (V5<jats:sub>180N</jats:sub>) rates and incubated for 7, 14, and 28 d. Even distribution of precipitation and warmer temperatures before soil sampling and greater soil organic matter (SOM) increased PMN<jats:sub>an</jats:sub>. Soil properties, including total C, SOM, and total N, had the strongest relationships with PMN<jats:sub>an</jats:sub> (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.40), followed by temperature (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.20) and precipitation (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.18) variables. The strength of the relationships between soil properties and PMN<jats:sub>an</jats:sub> from PP<jats:sub>0N</jats:sub>, V5<jats:sub>0N</jats:sub>, and V5<jats:sub>180N</jats:sub> varied by ≤10%. Including soil and weather in the model greatly increased PMN<jats:sub>an</jats:sub> predictability (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.69), demonstrating the interactive effect of soil and weather on N mineralization at different times during the growing season regardless of N fertilization. Delayed soil sampling (V5<jats:sub>0N</jats:sub>) and sampling after fertilization (V5<jats:sub>180N</jats:sub>) reduced PMN<jats:sub>an</jats:sub> predictability. However, longer PMN<jats:sub>an</jats:sub> incubations improved PMN<jats:sub>an</jats:sub> predictability from both V5 soil samplings closer to the PMN<jats:sub>an</jats:sub> predictability from PP<jats:sub>0N</jats:sub>, indicating the potential of PMN<jats:sub>an</jats:sub> from longer incubations to provide improved estimates of N mineralization when N fertilizer is applied.</jats:p></jats:sec><jats:sec><jats:title>Core Ideas</jats:title><jats:p><jats:list list-type="bullet"> <jats:list-item><jats:p>Relationships between mineralization estimates taken with the PMN<jats:sub>an</jats:sub> test and soil and weather conditions need to be improved.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil sample timing and N fertilization minimally affected PMN<jats:sub>an</jats:sub> predictability by soil and weather parameters.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil properties predict PMN<jats:sub>an</jats:sub> better than weather conditions.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil and weather conditions combined explain up to 69% of the variability of PMN<jats:sub>an</jats:sub>.</jats:p></jats:list-item> <jats:list-item><jats:p>Longer PMN<jats:sub>an</jats:sub> incubations improve the relationship between soil and weather parameters and PMN<jats:sub>an</jats:sub> after N fertilization.</jats:p></jats:list-item> </jats:list></jats:p></jats:sec> |
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imprint | Wiley, 2019 |
imprint_str_mv | Wiley, 2019 |
institution | DE-Brt1, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3 |
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issn_str_mv | 0361-5995, 1435-0661 |
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match_str | clark2019unitedstatesmidwestsoilandweatherconditionsinfluenceanaerobicpotentiallymineralizablenitrogen |
mega_collection | Wiley (CrossRef) |
physical | 1137-1147 |
publishDate | 2019 |
publishDateSort | 2019 |
publisher | Wiley |
record_format | ai |
recordtype | ai |
series | Soil Science Society of America Journal |
source_id | 49 |
spelling | Clark, Jason D. Veum, Kristen S. Fernández, Fabián G. Camberato, James J. Carter, Paul R. Ferguson, Richard B. Franzen, David W. Kaiser, Daniel E. Kitchen, Newell R. Laboski, Carrie A. M. Nafziger, Emerson D. Rosen, Carl J. Sawyer, John E. Shanahan, John F. 0361-5995 1435-0661 Wiley Soil Science http://dx.doi.org/10.2136/sssaj2019.02.0047 <jats:sec><jats:label /><jats:p>Nitrogen provided to crops through mineralization is an important factor in N management guidelines. Understanding of the interactive effects of soil and weather conditions on N mineralization needs to be improved. Relationships between anaerobic potentially mineralizable N (PMN<jats:sub>an</jats:sub>) and soil and weather conditions were evaluated under the contrasting climates of eight US Midwestern states. Soil was sampled (0–30 cm) for PMN<jats:sub>an</jats:sub> analysis before pre‐plant N application (PP<jats:sub>0N</jats:sub>) and at the V5 development stage from the pre‐plant 0 (V5<jats:sub>0N</jats:sub>) and 180 kg N ha<jats:sup>−1</jats:sup> (V5<jats:sub>180N</jats:sub>) rates and incubated for 7, 14, and 28 d. Even distribution of precipitation and warmer temperatures before soil sampling and greater soil organic matter (SOM) increased PMN<jats:sub>an</jats:sub>. Soil properties, including total C, SOM, and total N, had the strongest relationships with PMN<jats:sub>an</jats:sub> (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.40), followed by temperature (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.20) and precipitation (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.18) variables. The strength of the relationships between soil properties and PMN<jats:sub>an</jats:sub> from PP<jats:sub>0N</jats:sub>, V5<jats:sub>0N</jats:sub>, and V5<jats:sub>180N</jats:sub> varied by ≤10%. Including soil and weather in the model greatly increased PMN<jats:sub>an</jats:sub> predictability (<jats:italic>R</jats:italic><jats:sup>2</jats:sup> ≤ 0.69), demonstrating the interactive effect of soil and weather on N mineralization at different times during the growing season regardless of N fertilization. Delayed soil sampling (V5<jats:sub>0N</jats:sub>) and sampling after fertilization (V5<jats:sub>180N</jats:sub>) reduced PMN<jats:sub>an</jats:sub> predictability. However, longer PMN<jats:sub>an</jats:sub> incubations improved PMN<jats:sub>an</jats:sub> predictability from both V5 soil samplings closer to the PMN<jats:sub>an</jats:sub> predictability from PP<jats:sub>0N</jats:sub>, indicating the potential of PMN<jats:sub>an</jats:sub> from longer incubations to provide improved estimates of N mineralization when N fertilizer is applied.</jats:p></jats:sec><jats:sec><jats:title>Core Ideas</jats:title><jats:p><jats:list list-type="bullet"> <jats:list-item><jats:p>Relationships between mineralization estimates taken with the PMN<jats:sub>an</jats:sub> test and soil and weather conditions need to be improved.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil sample timing and N fertilization minimally affected PMN<jats:sub>an</jats:sub> predictability by soil and weather parameters.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil properties predict PMN<jats:sub>an</jats:sub> better than weather conditions.</jats:p></jats:list-item> <jats:list-item><jats:p>Soil and weather conditions combined explain up to 69% of the variability of PMN<jats:sub>an</jats:sub>.</jats:p></jats:list-item> <jats:list-item><jats:p>Longer PMN<jats:sub>an</jats:sub> incubations improve the relationship between soil and weather parameters and PMN<jats:sub>an</jats:sub> after N fertilization.</jats:p></jats:list-item> </jats:list></jats:p></jats:sec> United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen Soil Science Society of America Journal |
spellingShingle | Clark, Jason D., Veum, Kristen S., Fernández, Fabián G., Camberato, James J., Carter, Paul R., Ferguson, Richard B., Franzen, David W., Kaiser, Daniel E., Kitchen, Newell R., Laboski, Carrie A. M., Nafziger, Emerson D., Rosen, Carl J., Sawyer, John E., Shanahan, John F., Soil Science Society of America Journal, United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen, Soil Science |
title | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_full | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_fullStr | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_full_unstemmed | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_short | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
title_sort | united states midwest soil and weather conditions influence anaerobic potentially mineralizable nitrogen |
title_unstemmed | United States Midwest Soil and Weather Conditions Influence Anaerobic Potentially Mineralizable Nitrogen |
topic | Soil Science |
url | http://dx.doi.org/10.2136/sssaj2019.02.0047 |