The critical soil P levels for crop yield, soil fertility and environmental safety in different soil types
Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop y...
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| Published in | Plant and soil Vol. 372; no. 1/2; pp. 27 - 39 |
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| Main Authors | , , , , , , , , , , , |
| Format | Journal Article Conference Proceeding |
| Language | English |
| Published |
Dordrecht
Springer
01.11.2013
Springer Netherlands Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl₂-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg⁻¹ to 21.4 mg kg⁻¹, above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg⁻¹ to 90.2 mg kg⁻¹, above which soil CaCl₂-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg⁻¹ to 71.8 mg kg⁻¹ among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. |
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| AbstractList | Background and aims: Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods: Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl sub(2)-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results: The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg super(-1) to 21.4 mg kg super(-1), above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg super(-1) to 90.2 mg kg super(-1), above which soil CaCl sub(2)-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg super(-1) to 71.8 mg kg super(-1) among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions: The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. Background and aims: Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods: Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl2-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results: The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg-1 to 21.4 mg kg-1, above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg-1 to 90.2 mg kg-1, above which soil CaCl2-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg-1 to 71.8 mg kg-1 among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions: The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. © 2013 Springer Science+Business Media Dordrecht. Issue Title: In Memory of Horst Marschner Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl^sub 2^-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg^sup -1^ to 21.4 mg kg^sup -1^, above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg^sup -1^ to 90.2 mg kg^sup -1^, above which soil CaCl^sub 2^-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg^sup -1^ to 71.8 mg kg^sup -1^ among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field.[PUBLICATION ABSTRACT] Erratum DOI: 10.1007/s11104-013-1696-y Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl 2 -P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg −1 to 21.4 mg kg −1 , above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg −1 to 90.2 mg kg −1 , above which soil CaCl 2 -P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg −1 to 71.8 mg kg −1 among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and CaCl₂-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg kg⁻¹ to 21.4 mg kg⁻¹, above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg kg⁻¹ to 90.2 mg kg⁻¹, above which soil CaCl₂-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6 mg kg⁻¹ to 71.8 mg kg⁻¹ among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P losses and associated eutrophication of surface waters. The aim of this study was to determine critical soil P levels for achieving optimal crop yields and minimal P losses in common soil types and dominant cropping systems in China. Methods Four long-term experiment sites were selected in China. The critical level of soil Olsen-P for crop yield was determined using the linear-plateau model. The relationships between the soil total P, Olsen-P and Ca[Cl.sub.2]-P were evaluated using two-segment linear model to determine the soil P fertility rate and leaching change-point. Results The critical levels of soil Olsen-P for optimal crop yield ranged from 10.9 mg [kg.sup.-1] to 21.4 mg [kg.sup.-1], above which crop yield response less to the increasing of soil Olsen-P. The P leaching change-points of Olsen-P ranged from 39.9 mg [kg.sup.-1] to 90.2 mg [kg.sup.-1], above which soil Ca[Cl.sub.2]-P greatly increasing with increasing soil Olsen-P. Similar change-point was found between soil total P and Olsen-P. Overall, the change-point ranged from 4.6mg [kg.sup.-1] to 71.8 mg [kg.sup.-1] among all the four sites. These change-points were highly affected by crop specie, soil type, pH and soil organic matter content. Conclusions The three response curves could be used to access the soil Olsen-P status for crop yield, soil P fertility rate and soil P leaching risk for a sustainable soil P management in field. Keywords Critical level * Response curve * P leaching * Olsen-P * Ca[Cl.sub.2]-P |
| Audience | Academic |
| Author | Zhang, Fusuo Shen, Jianbo Bai, Zhaohai Li, Dongchu Wang, Boren Oenema, Oene Yang, Xueyun Li, Haigang Shi, Xiaojun Chen, Qing Zhou, Baoku Qin, Wei |
| Author_xml | – sequence: 1 givenname: Zhaohai surname: Bai fullname: Bai, Zhaohai – sequence: 2 givenname: Haigang surname: Li fullname: Li, Haigang – sequence: 3 givenname: Xueyun surname: Yang fullname: Yang, Xueyun – sequence: 4 givenname: Baoku surname: Zhou fullname: Zhou, Baoku – sequence: 5 givenname: Xiaojun surname: Shi fullname: Shi, Xiaojun – sequence: 6 givenname: Boren surname: Wang fullname: Wang, Boren – sequence: 7 givenname: Dongchu surname: Li fullname: Li, Dongchu – sequence: 8 givenname: Jianbo surname: Shen fullname: Shen, Jianbo – sequence: 9 givenname: Qing surname: Chen fullname: Chen, Qing – sequence: 10 givenname: Wei surname: Qin fullname: Qin, Wei – sequence: 11 givenname: Oene surname: Oenema fullname: Oenema, Oene – sequence: 12 givenname: Fusuo surname: Zhang fullname: Zhang, Fusuo |
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| Snippet | Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P... Background and aims Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P... Issue Title: In Memory of Horst Marschner Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may... Background and aims: Sufficient soil phosphorus (P) is important for achieving optimal crop production, but excessive soil P levels may create a risk of P... |
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| SubjectTerms | Acid soils Agricultural soils Agrology Agronomy. Soil science and plant productions Animal, plant and microbial ecology Biological and medical sciences Biomedical and Life Sciences Calcareous soils China Clay loam soils Crop production Crop yield Crop yields Cropping systems Crops Ecology Environment Environmental protection Eutrophication Fertilizers Fundamental and applied biological sciences. Psychology General agronomy. Plant production Leaching Life Sciences linear models long term experiments Nutrient management Organic matter phosphorus Phosphorus content Plant Physiology Plant Sciences Regular Article risk Silty soils Soil fertility Soil organic matter soil pH Soil science Soil Science & Conservation Soil types Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Soils Surface water |
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| Title | The critical soil P levels for crop yield, soil fertility and environmental safety in different soil types |
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