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Soil carbon (C), nitrogen (N) and phosphorus (P) stoichiometry drives phosphorus lability in paddy soil under long-term fertilization: A fractionation and path analysis study

文献类型： 外文期刊

作者： Qaswar, Muhammad 1 ; Ahmed, Waqas 1 ; Jing, Huang 1 ; Fan Hongzhu 3 ; Shi Xiaojun 4 ; Jiang Xianjun 4 ; Liu Kailou 1 ; Xu Yongmei 6 ; He Zhongqun 7 ; Asghar, Waleed 8 ; Shah, Asad 1 ; Zhang, Huimin 1 ;

作者机构： 1.Chinese Acad Agr Sci, Natl Engn Lab Improving Qual Arable Land, Inst Agr Resources & Reg Planning, Beijing, Peoples R China

2.Chinese Acad Agr Sci, Natl Observat Stn Qiyang Agriecol Syst, Inst Agr Resources & Reg Planning, Qiyang, Hunan, Peoples R China

3.Sichuan Acad Agr Sci, Soil & Fertilizer Res Inst, Chengdu, Sichuan, Peoples R China

4.Southwest Univ, Coll Resources & Environm, Chongqing, Peoples R China

5.Natl Engn & Technol Res Ctr Red Soil Improvement, Jiangxi Inst Red Soil, Nanchang, Jiangxi, Peoples R China

6.Xinjiang Acad Agr Sci, Inst Soil Fertilizer & Agr Water Conservat, Urumqi, Peoples R China

7.Sichuan Agr Univ, Coll Hort, Chengdu, Sichuan, Peoples R China

8.Beijing Normal Univ, Sch Environm, Beijing, Peoples R China

期刊名称：PLOS ONE （ 影响因子：3.24； 五年影响因子：3.788 ）

ISSN： 1932-6203

年卷期： 2019 年 14 卷 6 期

页码：

收录情况： SCI

摘要： Soil C:N:P stoichiometry plays a vital role in nutrient cycling in ecosystems, but its importance to P transformation in paddy soil remains unclear. We investigated the effect of soil C: N: P stoichiometry on P mobility and uptake under long-term fertilization. Three treatments, CK (no fertilization), NPK (inorganic nitrogen, phosphorus and potassium fertilization) and NPKM (combined inorganic NPK fertilizer and manure application), were selected from two long-term experiments of paddy soil that were initiated in 1991 and 1982 in Chongqing and Suining, respectively. The results showed that in comparison the control treatment, under long-term fertilization, soil pH decreased. In comparison with the NPK and CK treatments, the NPKM treatment significantly increased soil nutrient contents, P uptake and phosphatase activities. In comparison to the CK treatment, the NPK and NPKM treatments significantly decreased soil C: N, C: P and N: P ratios. In comparison to NPK and CK treatments, the NPKM treatment decreased residual-P at both sites. Compared with CK treatment, the NPKM treatments increased labile-P and moderately labile-P by 987% and 144%, respectively, and NPK treatment increased these factors by 823% and 125%, respectively, at the Chongqing site. At the Suining site, with NPKM treatment, increases in labile-P and moderately labile-P were 706% and 73%, respectively, and with NPK treatment, the increases were 529% and 47%, respectively. In contrast, non-labile-P was significantly decreased with NPKM treatment in comparison to that with NPK and CK treatments. Moreover, increases in soil C: N and C: P ratios decreased the labile-P pools and increased non-labile-P pools. A path analysis indicated that soil C: N: P stoichiometry indirectly controlled P uptake by directly affecting P transformation from non-labile to labile-P pools. Moreover, the non-labile-P in soil with high SOM and P content directly affected P uptake, indicating that soil P transformation is mainly driven by soil C and P in paddy soil. In conclusion, understanding mechanism of P mobility influenced by soil C:N:P stoichiometry could be helpful to manage soil P fertility under long-term fertilization in paddy soils of these regions.

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