不同研究尺度下土壤有机质和全氮的空间变异特征
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北京市教育委员会科技发展计划资助项目(KM-200510020006)


Spatial variability and distribution of soil organic matter and total nitrogen at different scales:a case study in Pinggu County,Beijing
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    摘要:

    在北京郊区面积为1075km2的中尺度(平谷区)以400m×400m网格采样,共采集1076个样点,同时在平谷区内面积为28.8km2的小尺度(马昌营镇)以100m×100m网格采样,共采集171个样点,测定其耕层土壤有机质和全氮的含量。应用传统统计学和地统计学方法,对两个研究尺度下的数据进行了分析,结果表明:有机质和全氮的变异系数范围为0.31~0.40,均属中等变异强度,随着研究尺度的缩小,土壤全氮的变异系数减少。半方差函数分析结果表明,两个研究尺度下,有机质和全氮均在一定范围内存在空间相关关系,区级尺度有机质和全氮的空间相关距离较大,分别为88.2 km和4.9 km,镇级尺度有机质和全氮的变程较小,均为0.7 km,它们的空间异质性均主要由结构性因素引起。采用Kriging最优内插法对未测点进行了估值,绘制了等值线图,两个研究尺度下的有机质和全氮含量受地形、土壤类型、土地利用方式、施肥等因素的影响,均表现出明显不同的分布规律。

    Abstract:

    Knowledge of spatial variability of soil organic matter (SOM) and total nitrogen (TN) at different scales is limited. The objective of this study was to assess the spatial variability of SOM and TN at two scales in the suburban of Beijing. Large-scale (county scale) topsoil samples (0-20 cm) were collected in a 400 m×400 m grid and a total of 1076 samples were taken within an area of 1075 km2 in Pinggu County. Small-scale (town scale) topsoil samples (0-20 cm) were collected in a 100 m×100 m grid and a total of 171 samples were taken within an area of 28.8 km2 in Machangying Town of the county. The contents of SOM and TN were determined for each soil sample. Descriptive statistics and geostatistics were used to analyze these two scales data. The results showed that the coefficients of variation (CV) for both SOM and TN variables at two scales were in the range of 0.31-0.40, which demonstrated a moderate variation among these. With the decreasing of scale, the CV for the TN content was reduced slightly. Semivariance analysis showed that both SOM and TN variables of the two different scales were spatially correlation at different lag distances. At the county scale, SOM and TN content had a large spatial correlation distance, which were 88.2 km and 4.9 km, respectively. However, the SOM and TN content at the town scale had the smaller spatial correlation distance, which were close to 0.7 km. The unobserved points were estimated and the contour map was obtained using the kriging method. The results indicated that the spatial distribution of SOM and TN content at two different scales was obviously different. The mainly affected factors were the topology, soil type, land use types and farming practices etc.

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王淑英,路苹,王建立,杨柳,杨凯,于同泉*.不同研究尺度下土壤有机质和全氮的空间变异特征.生态学报,2008,28(10):4957~4964

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