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应用生态学报 ›› 2010, Vol. 21 ›› Issue (04): 883-888.

• 研究报告 • 上一篇    下一篇

基于多光谱遥感影像的表层土壤有机质空间格局反演

张法升1,2;曲威1,2;尹光华1;刘作新1   

  1. 1中国科学院沈阳应用生态研究所| 沈阳 110016|2中国科学院研究生院| 北京 100049
  • 出版日期:2010-04-20 发布日期:2010-04-20

Spatial pattern of surface soil organic matter |based on remotely sensed multispectral image.

ZHANG Fa-sheng1,2;QU Wei1,2 |YIN Guang-hua1;LIU Zuo-xin1   

  1. 1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China|2Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2010-04-20 Published:2010-04-20

摘要: 利用多光谱LandSat TM遥感影像反演辽宁省阜新镇表层土壤有机质的空间格局,筛选出与土壤有机质分布相关的TM波段,分析并确定表层土壤有机质含量与TM1、TM2 、TM3、TM4、TM5、TM6、TM7波段亮度值(digital number, DN)的相关关系,建立了土壤有机质含量的光谱预测模型.结果表明:研究区表层土壤有机质含量与TM 4、TM 5波段DN值呈极显著的负相关关系(r分别为-0.617和-0.623,P<0.001),与TM 3、TM 5波段DN值之间满足负二次多项式回归关系(R2=0.9134,P<0.001);基于TM 3、TM 5波段DN值的回归模型对研究区表层土壤有机质含量的预测结果可靠(R2=0.9151,P<0.001).研究区表层土壤有机质含量<10 g·kg-1的农田主要分布在山地边缘地带,而平坦地区农田表层土壤有机质含量一般>10 g·kg-1,部分达到15~20 g·kg-1.

关键词: 多光谱TM影像, 土壤有机质, 空间格局, 大豆, 干旱, &alpha, -萘乙酸, 抗氧化系统

Abstract: Remotely sensed multispectral LandSat TM image was used to analyze the spatial pattern of surface soil organic matter across the cropland in Fuxin Town of Liaoning Province. The proper bands of the TM image that correlated with the distribution of surface soil organic matter were selected, and the quantitative relationships between surface soil organic matter and the digital number (DN) values of bands TM 1, TM 2, TM 3, TM 4, TM 5, TM 6, and TM 7 were analyzed and determined, which could be applied to establish a prediction model of surface soil organic matter. It was shown that the surface soil organic matter in study area had a strong negative correlation with the DN values of TM 4 and TM 5 (r=-0.617 and -0.623, P<0.001), and an inverse second order polynomial regression with the DN values of TM 3 and TM 5 (R2=09134, P<0.001). The regression model using the DN values of TM 3 and TM 5 could make a reliable prediction of the spatial pattern of surface soil organic matter (R2=0.9151, P<0.001). Across the study area, the cropland with soil organic matter content less than 10 g·kg-1 was mainly distributed in the zones at hill foot, while that with surface soil organic matter content usually more than 10 g·kg-1 and partly reached 15-20 g·kg-1 was in flat zone.

Key words: multispectral TM image, soil organic matter, spatial pattern, soybean, drought stress, NAA, antioxidant system.