王国芳, 张吴平, 毕如田, 张茜, 任健, 乔磊, 申若禹, 王佩浩. 县域尺度农田深层土壤有机质的估算及空间变异特征[J]. 农业工程学报, 2019, 35(22): 122-131. DOI: 10.11975/j.issn.1002-6819.2019.22.014
    引用本文: 王国芳, 张吴平, 毕如田, 张茜, 任健, 乔磊, 申若禹, 王佩浩. 县域尺度农田深层土壤有机质的估算及空间变异特征[J]. 农业工程学报, 2019, 35(22): 122-131. DOI: 10.11975/j.issn.1002-6819.2019.22.014
    Wang Guofang, Zhang Wuping, Bi Rutian, Zhang Qian, Ren Jian, Qiao Lei, Shen Ruoyu, Wang Peihao. Estimation and spatial variability of organic matter in deep soil of farmland at county scale[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(22): 122-131. DOI: 10.11975/j.issn.1002-6819.2019.22.014
    Citation: Wang Guofang, Zhang Wuping, Bi Rutian, Zhang Qian, Ren Jian, Qiao Lei, Shen Ruoyu, Wang Peihao. Estimation and spatial variability of organic matter in deep soil of farmland at county scale[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(22): 122-131. DOI: 10.11975/j.issn.1002-6819.2019.22.014

    县域尺度农田深层土壤有机质的估算及空间变异特征

    Estimation and spatial variability of organic matter in deep soil of farmland at county scale

    • 摘要: 县域是实施农业绿色发展的基本单元,农田土壤中不仅耕层的有机质含量会对土壤肥力产生影响,深层有机质的作用也不可忽略,精确估算基于县域尺度农田深层有机质含量具有重要意义。该研究选定位于山西省运城市的永济市农田为研究区,采用多点混合取样法,获取了8个样地剖面的18层数据,共144个混合土样的有机质含量数据,建立了表层(0~20 cm)有机质含量估算深层有机质含量的模型,并进行深层有机质含量的估算。基于半变异函数、空间自相关理论分析了0~30、>30~60、>60~90、>90~120、>120~150和>150~180 cm土层有机质含量的空间相关性和聚集特征,并进行了相关性检验,采用克里格插值方法对研究区农田各土层的有机质含量进行了预测。结果表明:1)土壤有机质含量随深度的增加呈负指数递减(R2=0.80,P<0.01),各土层的有机质含量变异系数介于35.89%~47.84%之间,处于中等变异程度。2)通过建立的估算模型可以通过表层有机质含量估算出任意深度的有机质含量,且拟合精度R2达到了0.90(P<0.01)。3)指数模型是反映该区域有机质含量空间结构特征的最佳模型(R2>0.80,RSS<0.001),各土层的有机质含量均表现出了中等程度结构性特征,和空间正相关性特征(Moran's I=0.26,P<0.01),并存在显著的空间聚集特征和异常值现象。4)克里格插值可以较好地进行研究区各层有机质含量的预测,预测精度较高,稳定性较好,为县域尺度深层有机质的估算,调整农艺措施、提高土壤肥力、达到土壤减肥增效、绿色增产增效提供依据。

       

      Abstract: Abstract: The county area is the basic unit for implementing green development of agriculture. In the farmland soil, not only the organic matter of the plough layer will affect the soil fertility, but also the role of deep organic matter can be neglected. Therefore, it is of great significance to accurately estimate the deep organic matter content of the farmland based on the county scale. This study selected the farmland in Yongji City, Yuncheng City, Shanxi Province as the research area. According to the soil types, 8 plots were determined, 3 vertical sections for each plot, and each vertical section was sampled by layer (10 cm for 1 layer). Three samples were randomly selected from each layer, and soil samples were mixed in the same layer. A mixed sample was formed, and a total of 18 layers of 180 cm depth were obtained, and a total of 144 samples were mixed. The organic matter content of each layer of soil was determined by the potassium dichromate volumetric method. A model for estimating the content of deep organic matter in the surface layer (0-20 cm) was established. Based on variogram and spatial autocorrelation, a total of 6 soil organic matters were analyzed from 0 to 30 cm, 30 to 60 cm, 60 to 90 cm, 90 to 120 cm, 120 to 150 cm and 150 to 180 cm. The spatial variability and clustering characteristics were tested and the correlation test was carried out. The Kriging interpolation method was used to predict the organic matter content of the farmland in the study area. The results showed that: 1) The content of soil organic matter decreased with the increase of depth and decreased with negative index (R2=0.80, P<0.01), and the rate of decline of soil organic matter content in the range of 0-60 cm was greater than that of 60-180 cm. The organic matter content data of each soil layer accorded with the normal distribution (P>0.05), which was moderately mutated. The degree of variation of organic matter in each layer was different, ranging from 35.89% to 47.84 %. 2) The organic matter content at any depth could be estimated by the surface organic matter content, and the fitting accuracy R2 =0.90 (P<0.01) , the error was less than 16%, accounting for 49.6%, and between 16% and 40%, accounting for 44.1%. 3) The index model was the best model to reflect the spatial structure of organic matter in this region (R2>0.80, RSS<0.001). The sill (C0/(C0+ C1)) of each soil layer in the study area was between 61.54% and 72.45%, which was moderately spatially correlated. The random factor contributed a lot to the spatial structure variation of organic matter content. 4) The global Moran index of Moran's I was 0.26, and the spatial distribution of organic matter content was positively correlated, and passed the 0.01 significance test. The organic matter content of farmland in the study area had high value clustering (High-High), low-valued aggregate (Low-Low), high value surrounded by low-valued (High-Low), and low-value surrounded by low-valued (Low-High). In space, it was characterized by low concentration of organic matter in the north and high concentration in the south. 5) Kriging interpolation could better predict the organic matter content of each layer in the study area, with high prediction accuracy and good stability. The prediction results showed that the organic matter content of the farmland layer (0-30 cm) in the study area was medium; and the organic matter contents of 30-60 and 60-90 cm were lower; the organic matters at a depth of 90-120, 120-150, 150 to 180 cm were very low. It could be seen that the organic matter content of the study area was not high and the soil fertility was moderate. It was an estimation of deep organic matter at the county scale, adjusting agronomic measures, improving soil fertility, and achieving soil weight loss and efficiency. The study provides a basis for green production and efficiency.

       

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