QANTITATIVE SPECTRAL ANALYSIS OF MAIN CLAY MINERALS IN SOIL

doi:10.6046/gtzyyg.1994.02.09

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Abstract

Abstract The clay mineralization and kaolinite enrichment in soil is one of the hydrocarbon’s Micro-Seepage characteristics. Study of the quantitative relationship between the clay mineral content and the reflectance spectrum of soil is more useful for the application of the Imaging Spectrometry in oil and gas exploration. In this paper we study quantitatively the relationship between the nearinfrared reflectance spectrum of soil and the concentration of the main clay minerals in soil. The estimation equations are derived with the relationship coefficient (R²)better than 0. 8.

Keywords Sanjiang plain Landscape pattern changes Land use/cover Remote sensing GIS

Issue Date: 02 August 2011

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	YE Bao-Ying
	ZHU Yan
	JI Wei
	ZHANG Yang-Zhen
	ZHANG Shu-Wen
	WANG Gao-Cheng
	GUO Ling
	CHEN Xin-Bing
	XU Lei
	TANG Lei

Cite this article:

YE Bao-Ying,ZHU Yan,JI Wei, et al. QANTITATIVE SPECTRAL ANALYSIS OF MAIN CLAY MINERALS IN SOIL[J]. REMOTE SENSING FOR LAND & RESOURCES, 1994, 6(2): 52-54，33.

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https://www.gtzyyg.com/EN/10.6046/gtzyyg.1994.02.09 OR https://www.gtzyyg.com/EN/Y1994/V6/I2/52

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