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Titlebook: Human Interference on River Health; A Study on the Haora Shreya Bandyopadhyay,Sunil Kumar De Book 2017 Springer International Publishing Sw

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41#
發(fā)表于 2025-3-28 18:22:48 | 只看該作者
42#
發(fā)表于 2025-3-28 19:00:32 | 只看該作者
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發(fā)表于 2025-3-29 01:52:55 | 只看該作者
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發(fā)表于 2025-3-29 04:56:40 | 只看該作者
nner of Being’s presence,. the traditional showing of Being itself — that as which Being reveals itself but such that this revealing is at once a self-concealing. Thus Being accords itself by not. according itself, and consequently the significance of the “negative” as self-preserving concealment, a
45#
發(fā)表于 2025-3-29 08:50:22 | 只看該作者
Haora River Basin: Location and Geographical Background,dated quaternary sediments. Most of the younger sediments are highly fragile and susceptible to erosion. From the cross-sectional study of the river, it is observed that within the survey period, the river is experiencing changes in its physical and social condition.
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發(fā)表于 2025-3-29 14:11:52 | 只看該作者
Status of Population Growth,trend of household distribution is showing a great variation within the entire basin. The growth of household in Agartala and Dukli areas always remains high, but households are still very less in the Baramura part of the river basin. The economic status of the Haora River basin is indicating a well
47#
發(fā)表于 2025-3-29 18:45:47 | 只看該作者
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發(fā)表于 2025-3-29 21:19:19 | 只看該作者
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發(fā)表于 2025-3-30 03:13:08 | 只看該作者
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發(fā)表于 2025-3-30 05:30:50 | 只看該作者
Estimation of Bank Erosion of the Haora River and Proposition of Bank Erosion Vulnerability Zonatioation. This zonation can be done by estimating eight parameters, i.e. (i) rainfall erosivity, (ii) lithological factor, (iii) slope of the river bank, (iv) meander index of each curve of the river, (v) river gradient (longitudinal), (vi) soil erodibility factor of the bank, (vii) vegetation cover of
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