Carbon, nitrogen, and phosphorus stoichiometry mediate sensitivity of carbon stabilization mechanisms along with surface layers of a Mollisol after long-term fertilization in Northeast China
文献类型: 外文期刊
作者: Abrar, Muhammad Mohsin 1 ; Xu, Hu 1 ; Aziz, Tariq 2 ; Sun, Nan 1 ; Mustafa, Adnan 1 ; Aslam, Muhammad Wajahat 3 ; Shah 1 ;
作者机构: 1.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Natl Engn Lab Improving Qual Arable Land, Beijing 100081, Peoples R China
2.Univ Agr Faisalabad, Inst Soil & Environm Sci, UAF Sub Campus Depalpur Okara, Faisalabad 38040, Pakistan
3.Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550081, Peoples R China
4.Nanjing Univ Informat Sci & Technol, China Meteorol Adm, Key Lab Aerosol Cloud Precipitat, Sch Atmospher Sci,Collaborat Innovat Ctr Forecast, Nanjing 210044, Jiangsu, Peoples R China
5.Heilongjiang Acad Agr Sci, Inst Environm & Resources, Harbin, Peoples R China
6.Henan Univ Sci & Technol, Coll Agr, Luoyang 471003, Henan, Peoples R China
7.Chinese Acad Trop Agr Sci CATAS, South Subtrop Crop Res Inst, Zhanjiang 524091, Guangdong, Peoples R China
关键词: Soil stoichiometry; Soil profile; Long-term fertilization; Protection mechanisms
期刊名称:JOURNAL OF SOILS AND SEDIMENTS ( 影响因子:3.308; 五年影响因子:3.586 )
ISSN: 1439-0108
年卷期:
页码:
收录情况: SCI
摘要: Purpose Soil organic carbon (SOC) is an important parameter determining soil fertility and sustaining soil health. How C, N, and P contents and their stoichiometric ratios (C/N/P) regulate the nutrient availability, and SOC stabilization mechanisms have not been comprehensively explored, especially in response to long-term fertilization. The present study aimed to determine how the long-term mineral and manure fertilization influenced soil C/N/P ratios and various protection mechanisms underlying the stabilization of OC along with profile in a cropland soil. Materials and methods The soil was sampled from five depths, viz., 0-20 cm, 20-40 cm, 40-60 cm, 60-80 cm, and 80-100 cm, from plots comprising wheat-maize-soybean rotation system subjected to the long-term (35 years) manure and mineral fertilizer applications. Results and discussion Results revealed that the soil C, N, P stoichiometry and their contents in topsoil depths (0-20 and 20-40 cm) and subsoil depths (40-60, 60-80, and 80-100 cm) varied significantly (p < 0.01) among the soil layers. Compared with CK, the C, N, and P contents were significantly higher (p < 0.05) in NPKM in the topsoil layers, while M alone increased these contents throughout the subsoil. Overall, the C, N, and P contents and their stoichiometry decreased with the increase in depth. Regression analysis showed that C/N, C/P, and N/P ratios associated significantly with the OC fractions in the topsoil layers only. These negative correlations indicated that these ratios significantly influence the C stabilization in the surface layers. However, the results warrant further investigations to study the relationship between soil and microbial stoichiometry and SOC at various depths. Conclusions Long-term manure applications improved the C sequestration not only in the topsoil but also in the deep layers; hence, these facts can be considered relevant for fertilizer recommendations in cropping systems across China.
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