检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:王佳盟 刘伟 刘志伟[1,2] 刘秀霞 吴秀兰 卞荣军 郑聚锋[1,2] 李恋卿 潘根兴[1,2] WANG Jia-meng;LIU Wei;LIU Zhi-wei;LIU Xiu-xia;WU Xiu-lan;BIAN Rong-jun;ZHENG Ju-feng;LI Lian-qing;PAN Gen-xing(Institute of Resource,Ecosystem and Environment of Agriculture,Nanjing Agricultural University,Nanjing 210095,China;Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization,Nanjing 210095,China)
机构地区:[1]南京农业大学农业资源与生态环境研究所,南京210095 [2]江苏省有机固体废弃物资源化协同创新中心,南京210095
出 处:《农业环境科学学报》2020年第9期2081-2088,共8页Journal of Agro-Environment Science
基 金:国家自然科学基金项目(41877097,41877096)。
摘 要:本文旨在揭示生物质炭施用下不同深度稻田土壤有机碳矿化特征的变化,为提高稻田土壤生物质炭施用下的固碳效应提供参考。以太湖地区施用生物质炭2 a后的水稻土为研究对象,采集了7个不同土壤深度的土壤样品,通过室内培养试验,分析了生物质炭施用下不同深度土壤有机碳分布及矿化特征。结果表明,生物质炭仅显著增加了表层(0~10 cm)土壤总有机碳含量,而对深层土壤无显著影响。然而,与对照相比,施用生物质炭显著降低了土壤0~40 cm有机碳矿化强度,0~10、10~20、20~30、30~40 cm土层的降幅分别为23.74%、37.57%、37.62%和15.95%,并降低了10~40 cm土层的微生物生物量碳和0~40 cm土层微生物代谢熵,同时表层(0~10 cm)土壤微生物生物量碳显著增加11.3%,而以上各指标在40 cm以下土层未因生物质炭添加而产生显著变化。因此,生物质炭在2 a尺度上提高了稻田土壤0~40 cm有机碳的稳定性,有助于增加深层土壤固碳潜力。This study aimed to clarify the effect of biochar on soil organic carbon mineralization characteristics of paddy soil at different depths and to provide a scientific basis for assessing the carbon sequestration effects of biochar in paddy soil.Soil samples were collected at seven different depths in a rice-cropping field located in Taihu Lake Region,which had received one dose of biochar two years ago.A labo⁃ratory experiment was conducted to analyze the organic carbon distribution and mineralization characteristics of the soil.The results showed that biochar application significantly increased the total organic carbon content in the surface layer(0~10 cm);however,it had no significant effect on the total organic carbon content in the layers below 10 cm.Compared with the control treatment,the biochar applica⁃tion significantly decreased the soil organic carbon mineralization intensity within the upper 40 cm layer.The decrease rate was 23.74%,37.57%,37.62%,and 15.95%for the 0~10 cm,10~20 cm,20~30 cm,and 30~40 cm layers,respectively.Biochar application significantly decreased the microbial biomass carbon in the 10~40 cm soil layer and the microbial metabolic quotient in the 0~40 cm soil layer,whereas the soil microbial biomass carbon in the surface layer(0~10 cm)was significantly increased by 11.3%in the biochar treatment.Below 40 cm layer,there was no significant change in any of the above indicators for biochar treatment.The results suggest that biochar application can improve the soil organic carbon stability within the 0~40 cm layer in paddy soil on a two-year scale,which is beneficial for the carbon sequestration potential in deep layers of the soil profile.
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:3.16.125.156