Acidification characteristics and its influencing factors of red paddy soil derived from four parent materials in Southeast of China
文献类型: 外文期刊
作者: Xie, Jun 1 ; Liang, Feng 1 ; Liu, Zengbing 2 ; Jiang, Guanjie 1 ; Zhang, Qin 1 ;
作者机构: 1.Jiangxi Agr Univ, Coll Land Resources & Environm, Key Lab Agr Resources & Ecol Poyang Lake Basin, Nanchang 330045, Jiangxi Provinc, Peoples R China
2.Jiangxi Acad Agr Sci, Inst Soil Fertilizer Resources & Environm, Nanchang 330200, Peoples R China
3.Jiangxi Agr Univ, Coll Land Resources & Environm, 1101 Zhimin Ave, Nanchang, Jiangxi Provinc, Peoples R China
关键词: Parent material; Red paddy soil (Ultisol); Acidification; Soil properties
期刊名称:GEODERMA REGIONAL ( 影响因子:4.1; 五年影响因子:3.9 )
ISSN: 2352-0094
年卷期: 2023 年 34 卷
页码:
收录情况: SCI
摘要: There are many types of parent materials of red paddy soil, however the acidification characteristics of paddy soil derived from different parent materials remain unclear in the past 40 years at Jiangxi Province, and the degree of soil properties on acidification is also still unknown. Therefore, four red paddy soil derived from Quaternary red earth (Qre), plate shale (P), red sand stone (Rs), granite (G) in Jiangxi Province was selected. We investigated the acidification characteristics and quantified the effect of soil factors on the acidification of red paddy soils derived from different parent materials. Results showed that related to the second soil survey (1980s), the pH of red paddy soil derived from four parent materials decreased by an average 0.47 unit, base saturation (BS%) decreased 13.93%, exchangeable acid (EA) and exchangeable aluminum (EAl) increased by 0.43 and 0.20 cmol center dot kg(-1), respectively. The Delta pH of red paddy soil derived from Rs (0.56) and G (0.54) were higher than that of Qre (0.34) and P (0.32). The Delta BS% of of red paddy soil derived from G (22.53%) > Rs (17.61%) > Qre (8.27%) > P (2.66%). The Delta EA (0.76) and Delta EAl (0.62) of Rs is highest. The results of redundancy analysis (RDA) shown that soil properties of red paddy soil derived from four parent material could explain 43.1% variation of soil acidification. CEC7, silt, sand, and SOM could explain 36.3%, 4.6%, 1.4% and 1.2% variation of acidification, respectively. The difference of soil mineralogy including oxide and clay minerals is also the reason for the different acidizing characteristics of paddy soil derived from four parent material. Therefore, compared with the 1980s, there is significant acidification of red paddy soil in 2018 in Jiangxi Province. The acidification of red paddy soil derived from red sand stone and granite is higher than that of plate shale and Quaternary red earth. And, parent material affect acidification by soil physicochemical and mineralogical properties.
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