资源评价

江汉平原县域尺度土壤有机质空间变异特征与合理采样数研究

展开
  • 华中师范大学 a. 地理过程分析与模拟湖北省重点实验室, b. 城市与环境科学学院,武汉 430079
于雷(1980- ),男,河南驻马店人,博士,中国自然资源学会会员(S300001769M),主要从事土壤地理学和土壤高光谱研究。E-mail:yulei@mail.ccnu.edu.cn

收稿日期: 2015-06-02

  修回日期: 2015-11-30

  网络出版日期: 2016-05-19

基金资助

国家自然科学基金项目(41401232,41271534); 中央高校基本科研业务费专项资金项目(CCNU15A05006,CCNU15ZD001)

Spatial Variability of Soil Organic Matter and Appropriate Number of Samples on County Scale in Jianghan Plain

Expand
  • a. College of City and Environmental Science, b. Key Laboratory for Geographical Process Analysis & Simulation, Hubei Province, Central China Normal University, Wuhan 430079, China

Received date: 2015-06-02

  Revised date: 2015-11-30

  Online published: 2016-05-19

Supported by

National Natural Science Foundation of China, No.41401232 and 41271534; Fundamental Research Funds for the Central Universities, No.CCNU15A05006 and CCNU15ZD001

摘要

土壤有机质含量是衡量土壤肥力和评价耕地质量的重要指标。在县域尺度下,利用合理数量的样点反映其空间分异特征具有重要意义。论文选取位于江汉平原腹地的湖北省公安县为研究区,布设了4 045个样点并测定其有机质含量,采用半方差分析得到土壤有机质空间变异特征,基于Moran’s I揭示空间变异较大地区,并通过二分法的思想逼近最佳合理采样数值。结果表明:研究区土壤有机质分布呈中等空间相关性,有6个局部区域的空间变异明显高于邻近地区,采样点数量与插值精度呈正相关,合理采样数为598个。研究结果可以为江汉平原县域耕地质量监测和管控提供指导。

本文引用格式

于雷, 魏东, 王惠霞, 黄群, 彭妍, 徐鸳媛 . 江汉平原县域尺度土壤有机质空间变异特征与合理采样数研究[J]. 自然资源学报, 2016 , 31(5) : 855 -863 . DOI: 10.11849/zrzyxb.20150614

Abstract

Soil organic matter (SOM) is a key index to estimate soil fertility and quality of cultivated land. Finding an appropriate number of samples on county scale is very important in saving costs while accurately expressing the spatial variability of SOM. In this research, Gong’an County, with an area of 2 258 km2, locating in the hinterland of Jianghan Plain (111°25′-111°48′E, 29°37′-30°19′N), was chosen as a typical case. A total of 4 045 soil samples were collected for analysis of SOM content. After the rejection of outliers, 3 950 sample sites were retained for further analysis. First, semi-variance function was used to explore the whole spatial variability. Then, a gradient template was defined to calculate the gradient vector, and the area was devided into seven parts based on the density of the pixels which had high gradient values. Moran’s I was used to describe the spatial variability of each part. In order to determine the appropriate number of samples, 100 points were randomly sampled and independent verification was used to validate the precision of Kriging interpolation result under different number of sample sites, i.e., 3 850, 2 695, 1 886, 1 320, 924, 647, 452 and 317. In order to improve the accuracy of sampling, a simple dichotomy method was employed to find the most appropriate number of samples. Geostatistical analysis suggested that the spatial variability of SOM distribution was moderate, and structural factors showed that SOM was affected by human activities in the research region. Six high spatially variated areas were found by gradient calculation on the basis of Kriging interpolation, and the local Moran’s I showed great anisotropy of SOM distribution and significant spatial variability in these regions, which suggested that more sampling sites are needed in these regions to obtain accurate spatial interpolation. Independent verification showed that the number of sampling points was positively correlated with the modeling accuracy and the reasonable number wasl was between 452 and 657 in this area. Finally, the appropriate sampling number was determined as 598 by dichotomy method. The results can provide guidance for monitoring and controling farmland quality in Jianghan Plain.

参考文献

[1] 赵明松, 张甘霖, 李德成, 等. 苏中平原南部土壤有机质空间变异特征研究 [J]. 地理科学, 2013, 33(1): 83-89.

[2] 王学锋, 章衡. 土壤有机质的空间变异性 [J]. 土壤, 1995(2): 85-89.

[3] 薛正平, 杨星卫, 段项锁, 等. 土壤养分空间变异及合理取样数研究 [J]. 农业工程学报, 2002, 18(4): 6-9.

[4] 阎波杰, 潘瑜春, 赵春江. 区域土壤重金属空间变异及合理采样数确定 [J]. 农业工程学报, 2008, 24(S2): 260-264.

[5] 赵倩倩, 赵庚星, 姜怀龙, 等. 县域土壤养分空间变异特征及合理采样数研究 [J]. 自然资源学报, 2012, 27(8): 1382-1391.

[6] 张志霞, 许明祥, 刘京, 等. 黄土高原不同地貌区土壤有机碳空间变异与合理取样数研究 [J]. 自然资源学报, 2014, 29(12): 2103-2113.

[7] 胡克林, 李保国, 林启美, 等. 农田土壤养分的空间变异性特征 [J]. 农业工程学报, 1999, 15(3): 33-38.

[8] 王军, 傅伯杰, 邱扬, 等. 黄土高原小流域土壤养分的空间异质性 [J]. 生态学报, 2002, 22(8): 1173-1178.

[9] 蒋勇军, 袁道先, 谢世友, 等. 典型岩溶流域土壤有机质空间变异——以云南小江流域为例 [J]. 生态学报, 2007, 27(5): 2040-2047.

[10] 韩丹, 程先富, 谢金红, 等. 大别山区江子河流域土壤有机质的空间变异及其影响因素 [J]. 土壤学报, 2012, 45(2): 403-408.

[11] 赵明松, 张甘霖, 王德彩, 等. 徐淮黄泛平原土壤有机质空间变异特征及主控因素分析 [J]. 土壤学报, 2013, 50(1): 1-11.

[12] 齐雁冰, 常庆瑞, 刘梦云, 等. 县域农田土壤养分空间变异及合理样点数确定 [J].土壤通报, 2014, 45(3): 556-561.

[13] 姜怀龙, 李贻学, 赵倩倩. 县域土壤有机质空间变异特征及合理采样数的确定 [J]. 水土保持通报, 2012, 32(4): 143-146.

[14] 宋莎, 李廷轩, 王永东, 等. 县域农田土壤有机质空间变异及其影响因素分析 [J]. 土壤, 2011, 43(1): 44-49.

[15] 张世文, 黄元仿, 苑小勇, 等. 县域尺度表层土壤质地空间变异与因素分析 [J]. 中国农业科学, 2011, 44(6): 1154-1164.

[16] 史文娇, 岳天祥, 石晓丽, 等. 土壤连续属性空间插值方法及其精度的研究进展 [J]. 自然资源学报, 2012, 27(1): 163-175.

[17] CRESSIE N, HAWKINS D M. Robust estimation of the variogram: I [J]. Journal of the International Association for Mathematical Geology, 1980, 12(2): 115-125.
[18] 胡伟, 邵明安, 王全九. 黄土高原退耕坡地土壤水分空间变异的尺度性研究 [J]. 农业工程学报, 2005, 21(8): 11-16.

[19] 宋同清, 彭晚霞, 曾馥平, 等. 喀斯特木论自然保护区旱季土壤水分的空间异质性 [J]. 应用生态学报, 2009, 20(1): 98-104.

[20] SHI W J, LIU J Y, DU Z P, et al. Surface modelling of soil pH [J]. Geoderma, 2009, 150(1/2): 113-119.
[21] SHI W J, LIU J Y, DU Z P, et al. Surface modelling of soil properties based on land use information [J]. Geoderma, 2011, 162(3): 347-357.
[22] 郭龙, 张海涛, 陈家赢, 等. 基于协同克里格插值和地理加权回归模型的土壤属性空间预测比较 [J]. 土壤学报, 2012, 49(5): 1037-1042.
文章导航

/