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摘要:
Soil samples were collected from eight basalt- derived chronosequence soils with the ages of 0.01, 0.58, 0.92, 1.33, 2.04, 3.04, 3.76 and 6.12 Ma respectively from Leizhou Peninsula and northern Hainan Island of tropical southern China. Magnetic parameters of magnetic susceptibility (MS), percentage of frequency-dependent magnetic susceptibility (FDS%), anhysteretic remanent magnetization (ARM), saturation isothermal remanent magnetization (SIRM), soft and hard isothermal remanent magnetization (IRMs and IRMh) of the collected samples were measured to study the evolution and the significance of the magnetism with soil age. The results show that the magnetic parameters changed fast from Primosols to Ferrosols (0.01 ~ 0.92 Ma) but slowly at Ferralosols stage (1.33 Ma~), it suggests a stable phase occurred for soil magnetism at Ferralosols, the existence of this phase could be supported by the little changes in the contents of clay, Fet and Fed. Obvious differences existed in the values of magnetic parameters between Ferralosols and other soil types (Primosols and Ferrosols), FDS%: Ferralosols > 10%, Primosols and Ferrosols –8· SIm3·kg–1, Primosols and Ferrosols > 8000 × 10–8 SIm3·kg–1, thus, it is possible to differentiate Ferralosols from other soil types in tropical region by using magnetic indices.
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篇名 Evolution and significance of soil magnetism of basalt-derived chronosequence soils in tropical southern China
来源期刊 农业科学(英文) 学科 医学
关键词 Magnetic Parameters Basalt-Derived CHRONOSEQUENCE Soil Iron OXIDES TROPICAL Southern China
年,卷(期) 2011,(4) 所属期刊栏目
研究方向 页码范围 536-543
页数 8页 分类号 R73
字数 语种
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Magnetic
Parameters
Basalt-Derived
CHRONOSEQUENCE
Soil
Iron
OXIDES
TROPICAL
Southern
China
研究起点
研究来源
研究分支
研究去脉
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相关学者/机构
期刊影响力
农业科学(英文)
月刊
2156-8553
武汉市江夏区汤逊湖北路38号光谷总部空间
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1151
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