中文关键词余干县土壤碳氮比时空变异成土母质氮肥施用量 英文关键词Yugan Countysoil carbon-to-nitrogen ratiospatial and temporal variabilityparent materialnitrogen fertilizer rate

作者	单位	E-mail
江叶枫	江西农业大学国土资源与环境学院, 南昌 330045 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045	jiangyf0308@163.com
钟珊	江西农业大学国土资源与环境学院, 南昌 330045 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045
李婕	江西农业大学国土资源与环境学院, 南昌 330045 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045
王澜珂	江西农业大学国土资源与环境学院, 南昌 330045 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045
郭熙	江西农业大学国土资源与环境学院, 南昌 330045 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045	xig435@163.com

中文摘要 基于1982年余干县第二次土壤普查200个样点数据和2012年测土配方施肥项目423个样点数据，运用方差分析、相关性分析、回归分析和普通克里格法，结合成土母质、土壤类型、耕地利用方式、地形因子、pH、秸秆还田和氮肥施用量，探讨近30年来余干县耕地表层（0~20 cm）土壤碳氮比（C/N）时空变异特征及其影响因素.结果表明余干县1982年和2012年土壤C/N均值依次为10.05和11.18，变异系数分别为19.40%和25.04%，均呈中等程度的变异性.经半变异函数分析，块金效应值分别为15.91%和71.25%，表明土壤C/N由结构性因素和随机性因素共同作用变为更倾向于受随机性因素的主导作用.近30年来大部分区域土壤C/N增加明显，以东部区域增加最为显著.1982年土壤C/N空间变异主要受成土母质、土壤类型、地形因子和pH的影响，其影响程度依次为17.3%、14.2%、7.4%和2.3%.2012年土壤C/N空间变异受成土母质、土壤类型、耕地利用方式、地形因子、秸秆还田和氮肥施用量共同作用，其影响程度依次为8.7%、23.5%、28.2%、12.2%、12.6%和42.3%. 英文摘要 The soil carbon-to-nitrogen (C/N) ratio of soils is a sensitive indicator of soil quality and an indicator for assessing the carbon and nitrogen nutrition balance of soils. Its variation is significant in reflecting the carbon and nitrogen cycling of soils. An accurate knowledge of how the C/N ratio varies spatially and temporally and the driving factors at county scale is of great significance to the extrapolation of balanced fertilization based on soil C/N ratio regulation as well as to the protection of the ecological environment. This study was based on 200 points of surface soil samples (0-20 cm) collected during the second National Soil Survey in 1982 and 423 points of surface soil samples (0-20 cm) collected during the soil test-based formulated fertilization project in 2012 in Yugan County. Combined with the soil parent material, soil type, farmland-use type, terrain factors, pH, straw incorporation pattern, and nitrogen fertilizer rate over the past 30 years, spatial and temporal variability characteristics of the soil C/N ratio were analyzed by using ordinary kriging methods, and the effects of the influencing factors were quantified by regression analysis. The results indicated that the mean value of the C/N ratio was 10.05 and 11.18 in 1982 and 2012, respectively. The coefficient of variation was 19.40% and 25.04%, respectively, which suggested the soil C/N ratio had moderate variability in the study area. The ratios of nugget to sill were 15.91% and 71.25% in 1982 and 2012, respectively. This means that the leading factor from the structural factors (parent material and soil type) into the stochastic factors (nitrogen fertilizer rate and straw incorporation pattern). In the past 30 years, most of the regional soil C/N ratio increased significantly especially the eastern region. The spatial variability of soil C/N in 1982 was mainly affected by soil parent material, soil type, terrain factor, and pH, with the degree of influence of each variable at 17.3%, 14.2%, 7.4%, and 2.3%. In 2012, the spatial variability was mainly affected by soil parent material, soil type, farmland-use type, terrain factor, straw incorporation pattern, and nitrogen fertilizer rate, with the degree of influence of each variable of 8.7%, 23.5% 28.2%, 12.2%, 12.6%, and 42.3%, respectively. To maintain the steady growth of the soil C/N ratio, it is suggested that the return of carbon be incorporated with the input of nitrogen, such as incorporating crop residues into the soil and inputting more organic fertilizers into the soil in future farming practices.

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