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Replacing nitrogen in mineral fertilizers with nitrogen in maize straw increases soil water-holding capacity.
Wang, Xiaojuan; Tian, Le; Wang, Tianle; Zhang, Enhui.
Affiliation
  • Wang X; Shanxi Institute of Organic Dryland Farming, Shanxi Agricultural University, Taiyuan, 030031, Shanxi, People's Republic of China. juanwxj@126.com.
  • Tian L; College of Agriculture, Shanxi Agricultural University, Taigu, 030801, Shanxi, People's Republic of China. juanwxj@126.com.
  • Wang T; State Key Laboratory of Integrative Sustainable Dryland Agriculture (in Preparation), Shanxi Agricultural University, Taiyuan, 030031, Shanxi, People's Republic of China. juanwxj@126.com.
  • Zhang E; Key Laboratory of Sustainable Dryland Agriculture (Co-Construction By Ministry of Agriculture and Rural Affairs and Shanxi Province), Shanxi Agricultural University, Taiyuan, 030031, Shanxi, People's Republic of China. juanwxj@126.com.
Sci Rep ; 14(1): 9337, 2024 Apr 23.
Article in En | MEDLINE | ID: mdl-38653762
ABSTRACT
Soil water-holding capacity decreases due to long-term mineral fertilizer application. The objective of this study was to determine how replacing mineral fertilizer with maize straw affected the soil water retention curve, soil water content, soil water availability, and soil equivalent pore size. Replacement treatments in which 25% (S25), 50% (S50), 75% (S75), and 100% (S100) of 225 kg ha-1 nitrogen from mineral fertilizer (CK) was replaced with equivalent nitrogen from maize straw were conducted for five years in the Loess Plateau of China. The Gardner model was used to fit the soil water retention curve and calculate the soil water constant and equivalent pore size distribution. The results indicated that the Gardner model fitted well. Replacing nitrogen from mineral fertilizer with nitrogen from straw increased soil specific water capacity, soil readily available water, soil delayed available water, soil available water, soil capillary porosity, and soil available water porosity over time. S25 increased field capacity and wilting point from the fourth fertilization year. S50 enhanced soil readily available water, soil delayed available water, soil available water, and soil available water porosity from the fifth fertilization year, whereas S25 and S75 increased these from the third fertilization year or earlier. Soil specific water capacity, soil readily available water, soil delayed available water, soil available water, soil capillary porosity, and soil available water porosity could better reflect soil water-holding capacity and soil water supply capacity compared with field capacity and wilting point.
Key words

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Rep Year: 2024 Document type: Article Country of publication: United kingdom

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Rep Year: 2024 Document type: Article Country of publication: United kingdom