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不同盐渍化土壤N2O排放对生物炭添加和土壤水分的响应
引用本文:王春,张通港,罗敏,闫思慧,程煜,张体彬,冯浩.不同盐渍化土壤N2O排放对生物炭添加和土壤水分的响应[J].干旱地区农业研究,2023(3):142-149.
作者姓名:王春  张通港  罗敏  闫思慧  程煜  张体彬  冯浩
作者单位:西北农林科技大学旱区农业水土工程教育部重点实验室,陕西 杨凌 712100;西北农林科技大学水利与建筑工程学院,陕西 杨凌 712100;西北农林科技大学旱区农业水土工程教育部重点实验室,陕西 杨凌 712100;西北农林科技大学水土保持研究所,陕西 杨凌 712100;中国科学院水利部水土保持研究所,陕西 杨凌 712100
基金项目:国家重点研发计划项目(2021YFD1900700);陕西省创新能力支撑计划项目(2022PT-23)
摘    要:为探讨不同盐渍化程度土壤N2O排放对生物炭添加和土壤水分的响应,开展为期30 d的室内培养试验,设置5个土壤盐渍化水平(S0、S1、S2、S3、S4:盐分添加量分别为土壤质量的0%、0.25%、0.5%、0.75%、1%)、2个生物炭添加方式(B0:不添加;B1:添加量为土壤质量的5%)和2个水分条件(W0:60%田间持水量;W1:100%田间持水量)。结果表明:土壤盐分对N2O累积排放量具有显著影响,盐分含量越高则降幅越大,与S0处理相比,S1、S2、S3、S4处理N2O累积排放量分别降低43.9%、66.5%、91.9%、93.2%。土壤水分对N2O累积排放量具有极显著影响,水分含量越高则累积排放量越大,与W0处理相比,W1条件下各盐分处理N2O累积排放量分别增加3.0%、84.8%、187.4%、729.4%、306.7%。生物炭添加对N2O累积排放量存在一定影响,与B0处理相比,低水含量下,B1处理累积排放量增幅为3.4%~20.6%,高水含量增幅...

关 键 词:盐渍化土壤  水分含量  生物炭  N2O排放

Response of soil N2O emission to biochar addition and water content under different salinization conditions
WANG Chun,ZHANG Tonggang,LUO Min,YAN Sihui,CHENG Yu,ZHANG Tibin,FENG Hao.Response of soil N2O emission to biochar addition and water content under different salinization conditions[J].Agricultural Research in the Arid Areas,2023(3):142-149.
Authors:WANG Chun  ZHANG Tonggang  LUO Min  YAN Sihui  CHENG Yu  ZHANG Tibin  FENG Hao
Institution:Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A&F University, Yangling, Shaanxi 712100, China; College of Water Resources and Architectural Engineering, Northwest A&F University, Yangling, Shaanxi 712100, China;Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A&F University, Yangling, Shaanxi 712100, China; Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China
Abstract:To investigate the response of soil N2O emission to biochar addition and soil water with different salinization levels, an indoor culture experiment was conducted for 30 days and five soil salinization levels (S0, S1, S2, S3 and S4) were set up. The salt content was 0%, 0.25%, 0.5%, 0.75% and 1% of soil mass, respectively. Two biochar addition modes of B0: no addition and B1: 5% of soil mass and 2 moisture conditions of W0: 60% field capacity and W1:100% field capacity were used. The results showed that soil salt had a significant effect on the cumulative emission of N2O, and the higher the salt content was, the greater the decrease was. Compared with S0 treatment, the cumulative emission of N2O in S1, S2, S3 and S4 treatments decreased by 43.9%, 66.5%, 91.9% and 93.2%, respectively. Soil moisture had a significant impact on the cumulative emission of N2O. The higher the moisture content was, the greater the cumulative emission was. Compared with W0 treatment, the cumulative emission of N2O in each salt treatment under W1 condition increased by 3.0%, 84.8%, 187.4%, 729.4% and 306.7%, respectively. The addition of biochar had an impact on the cumulative emission of N2O. Compared with B0 treatment, the increase of B1 in low water content was 3.4% to 20.6%, and that in high water content was 46.5% to 535.6%. The results showed that the higher the degree of salinization was, the lower the cumulative emissions of soil N2O became. Water had the dominant role in the emission of N2O as water had a very significant impact on the cumulative emissions of N2O. The higher the water content was, the higher the increase of cumulative emissions of N2O became. Biochar alone had no significant impact on the cumulative emissions of N2O. However, the interaction with salt had a significant effect on the cumulative emission of N2O, reducing the emission to a certain extent.
Keywords:salinized soil  water content  biochar  N2O emission
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