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- W2364890544 abstract "The character of soil magnetic susceptibility in the different parts of the slope, the mechanism of soil magnetic susceptibility changing after rain, and the feasibility of using magnetic tracer to study soil erosion are discussed based on the measurement of soil magnetic susceptibility in the slope, the desperation of different particle diameter range soil, and magnetic susceptibility measurement of different particle diameter soil, and using magnetic tracer to study soil erosion in the slope of a small watershed. The results of the experiment show that the soil magnetic susceptibility in the upper part of the slope is the lowest, the soil magnetic susceptibility in the middle part of the slope is the highest, and the soil magnetic susceptibility in the lower part of the slope is medium. The magnetic susceptibility of the separate whose particle diameter range is 0.1～0.25 mm is highest, the relationship between the magnetic susceptibility of this separate of the soil and the soil magnetic susceptibility is very significant. After raining, the soil magnetic susceptibility of the different parts of the slope changed much,its mechanism is that the magnetic mineral content of the soil in the slope changed after the soil eroded. The results of the tracing experiment show that the method of using magnetic tracer to study soil erosion in the slope is effective too." @default.
- W2364890544 created "2016-06-24" @default.
- W2364890544 creator A5087356446 @default.
- W2364890544 date "2004-01-01" @default.
- W2364890544 modified "2023-09-28" @default.
- W2364890544 title "Magnetic Susceptibility of Soil Eroded in Slope and Experiment of Magnetic Tracing on Slope Soil Erosion" @default.
- W2364890544 hasPublicationYear "2004" @default.
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