Effect of Soil Drying Intensity During an Experimental Drying-Rewetting Event on Nutrient Transformation and Microbial Community Composition  

作　　者：SUN Dashend BI Qingfang LI Kejie ZHU Jun ZHANG Qichun JIN Chongwei LU Lingli LIN Xianyong 

机构地区：[1]College of Resources and Environment, Shanxi Agricultural University, Taigu 030801 ,China [2]Key Laboratory of Environment Remediation and Ecological Health, Ministry of Education, College of Environmental & ResourceSciences, Zhejiang University, Hangzhou 310058 ,China [3]Institute of Soil and Water Resources and Environment, Zhejiang University, Hangzhou 310058 ,China [4]Key Laboratory of Subtropical Soil Science and Plant Nutrition of Zhejiang Province, College of Environmental & Resource Sciences,Zhejiang University, Hangzhou 310058 ,China

出　　处：《Pedosphere》2018年第4期644-655,共12页土壤圈（英文版）

基　　金：supported by the Scientific and Technological Innovation Fund of Shanxi Agricultural University,China(No.2017YJ17);the Outstanding Doctor Funding Award of Shanxi Province,China(No.SXYBKY201720);the National Basic Research Program(973 Program)of China(No.2013CB127403);the Strategic Priority Research Program of Chinese Academy of Sciences(No.XDB15020402);the National Natural Science Foundation of China(No.41571130061)

摘　　要：Soil drying-rewetting(DRW) events affect nutrient transformation and microbial community composition; however, little is known about the influence of drying intensity during the DRW events. Therefore, we analyzed soil nutrient composition and microbial communities with exposure to various drying intensities during an experimental drying-rewetting event, using a silt loam from a grassland of northern China, where the semi-arid climate exposes soils to a wide range of moisture conditions, and grasslands account for over 40% of the nation's land area. We also conducted a sterilization experiment to examine the contribution of soil microbes to nutrient pulses. Soil drying-rewetting decreased carbon(C) mineralization by 9%–27%. Both monosaccharide and mineral nitrogen(N) contents increased with higher drying intensities(drying to ≤ 10% gravimetric water content), with the increases being 204% and 110% with the highest drying intensity(drying to 2% gravimetric water content), respectively, whereas labile phosphorus(P)only increased(by 105%) with the highest drying intensity. Moreover, levels of microbial biomass C and N and dissolved organic N decreased with increasing drying intensity and were correlated with increases in dissolved organic C and mineral N, respectively,whereas the increases in labile P were not consistent with reductions in microbial biomass P. The sterilization experiment results indicated that microbes were primarily responsible for the C and N pulses, whereas non-microbial factors were the main contributors to the labile P pulses. Phospholipid fatty acid analysis indicated that soil microbes were highly resistant to drying-rewetting events and that drought-resistant groups were probably responsible for nutrient transformation. Therefore, the present study demonstrated that moderate soil drying during drying-rewetting events could improve the mineralization of N, but not P, and that different mechanisms were responsible for the C, N, and P pulses observed during drying-rewetting events.Soil drying-rewetting （DRW） events affect nutrient transformation and microbial community composition; however, little is known about the influence of drying intensity during the DRW events. Therefore, we analyzed soil nutrient composition and microbial communities with exposure to various drying intensities during an experimental drying-rewetting event, using a silt loam from a grassland of northern China, where the semi-arid climate exposes soils to a wide range of moisture conditions, and grasslands account for over 40% of the nation＇s land area. We also conducted a sterilization experiment to examine the contribution of soil microbes to nutrient pulses. Soil drying-rewetting decreased carbon （C） mineralization by 9%-27%. Both monosaccharide and mineral nitrogen （N） contents increased with higher drying intensities （drying to ≤ 10% gravimetric water content）, with the increases being 204% and 110% with the highest drying intensity （drying to 2% gravimetric water content）, respectively, whereas labile phosphorus （P） only increased （by 105%） with the highest drying intensity. Moreover, levels of microbial biomass C and N and dissolved organic N decreased with increasing drying intensity and were correlated with increases in dissolved organic C and mineral N, respectively, whereas the increases in labile P were not consistent with reductions in microbial biomass P. The sterilization experiment results indicated that microbes were primarily responsible for the C and N pulses, whereas non-microbial factors were the main contributors to the labile P pulses. Phospholipid fatty acid analysis indicated that soil microbes were highly resistant to drying-rewetting events and that drought-resistant groups were probably responsible for nutrient transformation. Therefore, the present study demonstrated that moderate soil drying during drying-rewetting events could improve the mineralization of N, but not P, and that different mechanisms were responsible for the C, N, and P pulses observed dur

关 键 词：drought-resistant microbial groups gravimetric water content microbial biomass nutrient mineralization nutrient pulse soil microbes soil respiration 

分 类 号：S154.3[农业科学—土壤学] TP311.13[农业科学—农业基础科学]