Impact of soil moisture regimes on greenhouse gas emissions, soil microbial biomass, and enzymatic activity in long-term fertilized paddy soil

被引:7
|
作者
Shah, Asad [1 ]
Huang, Jing [1 ,2 ]
Han, Tianfu [1 ]
Khan, Muhammad Numan [3 ]
Tadesse, Kiya Adare [1 ]
Daba, Nano Alemu [1 ]
Khan, Sajeela [4 ]
Ullah, Sami [5 ]
Sardar, Muhammad Fahad [5 ]
Fahad, Shah [6 ,7 ]
Zhang, Huimin [1 ,2 ]
机构
[1] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, State Key Lab Efficient Utilizat Arid & Semiarid A, Beijing 100081, Peoples R China
[2] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Natl Observat Stn Qiyang Agriecol Syst, Qiyang 426182, Hunan, Peoples R China
[3] Chinese Acad Sci, CAS Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Menglun 666303, Yunnan, Peoples R China
[4] Abdulwali Khan Univ, Dept Bot, Mardan, KPK, Pakistan
[5] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Minist Agr Key Lab Plant Nutr & Fertilizer, Beijing, Peoples R China
[6] Shandong Univ, Sch Life Sci, Key Lab Ecol Prewarning Protect & Restorat Bohai S, Minist Nat Resources, Qingdao 266237, Peoples R China
[7] Abdulwali Khan Univ, Coll Agr, Mardan, KPK, Pakistan
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Greenhouse gas emissions; Microbial biomass stoichiometry; Soil enzymes; Moisture content; Long-term fertilization; NITROUS-OXIDE EMISSIONS; ORGANIC-MATTER; N2O EMISSIONS; P STOICHIOMETRY; CH4; EMISSIONS; ACIDIC SOILS; RICE; METHANE; WATER; COMMUNITIES;
D O I
10.1186/s12302-024-00943-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Two potent greenhouse gases that are mostly found in agricultural soils are methane and nitrous oxide. Therefore, we investigated the effect of different moisture regimes on microbial stoichiometry, enzymatic activity, and greenhouse gas emissions in long-term paddy soils. The treatments included a control (CK; no addition), chemical fertilizer (NPK), and NPK + cattle manure (NPKM) and two moisture regimes such as 60% water-filled pore spaces (WFPS) and flooding. The results revealed that 60% water-filled pore spaces (WFPS) emit higher amounts of N2O than flooded soil, while in the case of CH4 the flooded soil emits more CH4 emission compared to 60% WFPS. At 60% WFPS higher N2O flux values were recorded for control, NPK, and NPKM which are 2.3, 3.1, and 3.5 mu g kg-1, respectively. In flooded soil, the CH4 flux emission was higher, and the NPKM treatment recorded the maximum CH4 emissions (3.8 mu g kg-1) followed by NPK (3.2 mu g kg-1) and CK (1.7 mu g kg-1). The dissolved organic carbon (DOC) was increased by 15-27% under all flooded treatments as compared to 60% WPFS treatments. The microbial biomass carbon, nitrogen, and phosphorus (MBC, MBN, and MBP) significantly increased in the flooded treatments by 8-12%, 14-21%, and 4-22%, respectively when compared to 60% WFPS. The urease enzyme was influenced by moisture conditions, and significantly increased by 42-54% in flooded soil compared with 60% WFPS while having little effect on the beta-glucosidase (BG) and acid phosphatase (AcP) enzymes. Moreover DOC, MBC, and pH showed a significant positive relationship with cumulative CH4, while DOC showed a significant relationship with cumulative N2O. In the random forest model, soil moisture, MBC, DOC, pH, and enzymatic activities were the most important factors for GHG emissions. The PLS-PM analysis showed that soil properties and enzymes possessed significantly directly impacted on CH4 and N2O emissions, while SMB had indirect positive effect on CH4 and N2O emissions.
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页数:12
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