长江沉积物中赤铁矿和针铁矿的漫反射光谱分析

李超; 杨守业

doi:10.3799/dqkx.2012.S1.002

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LI Chao, YANG Shou-ye, 2012. Hematite and Goethite Distribution in the Yangtze River Sediments by Using Diffused Reflectance Spectroscopy. Earth Science, 37(S1): 11-19. doi: 10.3799/dqkx.2012.S1.002

Citation:

LI Chao, YANG Shou-ye, 2012. Hematite and Goethite Distribution in the Yangtze River Sediments by Using Diffused Reflectance Spectroscopy. Earth Science, 37(S1): 11-19. doi: 10.3799/dqkx.2012.S1.002

LI Chao, YANG Shou-ye, 2012. Hematite and Goethite Distribution in the Yangtze River Sediments by Using Diffused Reflectance Spectroscopy. Earth Science, 37(S1): 11-19. doi: 10.3799/dqkx.2012.S1.002

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Hematite and Goethite Distribution in the Yangtze River Sediments by Using Diffused Reflectance Spectroscopy

doi: 10.3799/dqkx.2012.S1.002

LI Chao^1
,,
YANG Shou-ye²

1.
School of Ocean and Earth Sciences, Tongji University, Shanghai 200092, China
2.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

Received Date: 2011-10-01
Available Online: 2021-11-15
Publish Date: 2012-05-01

Abstract

Abstract

As two common weathering minerals, hematite and goethite are generally regarded as sensitive indicators for environment. In this paper, suspended particle matter and floodplain sediments from the main stream and major tributaries of the Yangtze River are systemically studied by diffuse reflectance spectroscopy (DRS). The result reveals that the first derivative curve peak for hematite in the Yangtze River sediments occurs at 565 nm, while the first derivative curve main peak for goethite occurs at 505 nm and secondary peak for goethite occurs at 435 nm. It is different from previous studies on loess that the height of goethite's main peak in the Yangtze River sediments is overall higher than its secondary peak. In the Yangtze River catchment, both hematite and goethite are quite homogeneous in the Yangtze River main stream due to the hydrodynamic mixing, while variations in hematite and goethite contents are larger in the tributaries. Clear differences in DRS are observed between the Yangtze River and Huanghe sediments, loess and dust, which implies that the DRS method may shed new light on discriminating sediment provenances.
- hematite,
- goethite,
- diffuse reflectance spectroscopy,
- Yangtze River,
- sediments,
- source tracer,
- mineralogy

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References(44)

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Hematite and Goethite Distribution in the Yangtze River Sediments by Using Diffused Reflectance Spectroscopy

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