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Soil-environmental relationships on the Brahmaputra and Ganges floodplains in Bangladesh
The reconnaissance soil survey of Pakistan 1961-71 produced important new information on the environmental relationships of soils on the Brahmaputra and Ganges floodplains in East Pakistan (now Bangladesh) which provided a sound basis for agricultural land use planning in the country. The greater pa...
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Published in: | International journal of environmental studies 2022-09, Vol.79 (5), p.935-950 |
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description | The reconnaissance soil survey of Pakistan 1961-71 produced important new information on the environmental relationships of soils on the Brahmaputra and Ganges floodplains in East Pakistan (now Bangladesh) which provided a sound basis for agricultural land use planning in the country. The greater part of the territory was found to have been formed in sediments deposited by tributary and distributary rivers, not by the two major rivers themselves. Piedmont, river meander, estuarine and tidal floodplain landscapes of different ages were recognised, with intricate relief and soil patterns with associated local differences in land use and crop suitability. In all except current active floodplain and piedmont fan areas, seasonal flooding was found to be mainly by rainwater ponded on the floodplains by high seasonal flood levels in the major rivers flowing into the country. Therefore, the country's floodplains are not occupied, as is popularly believed, by sediments receiving annual increments of fertile alluvium; they are mainly occupied by soils developed to different degrees according to differences in sediment origin and landscape age, with profiles reflecting local differences in relief and drainage, and further changed by degradation through ferrolysis and by puddling of topsoils for rice cultivation. |
doi_str_mv | 10.1080/00207233.2021.1974755 |
format | article |
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Therefore, the country's floodplains are not occupied, as is popularly believed, by sediments receiving annual increments of fertile alluvium; they are mainly occupied by soils developed to different degrees according to differences in sediment origin and landscape age, with profiles reflecting local differences in relief and drainage, and further changed by degradation through ferrolysis and by puddling of topsoils for rice cultivation.</description><identifier>ISSN: 0020-7233</identifier><identifier>EISSN: 1029-0400</identifier><identifier>DOI: 10.1080/00207233.2021.1974755</identifier><language>eng</language><publisher>New York: Routledge</publisher><subject>Agricultural land ; Alluvial deposits ; Alluvium ; Bangladesh ; Cultivation ; Environmental science ; Environmental studies ; Estuaries ; ferrolysis ; Flood levels ; Flooding ; floodplain soil ; Floodplains ; Foothills ; Grain cultivation ; Land use ; Land use management ; Land use planning ; Landscape ; paddy soil ; Puddling ; Rain water ; Rivers ; Sediments ; soil coatings ; Soil surveys ; Soils ; Tidal floods ; toposequence ; Topsoil</subject><ispartof>International journal of environmental studies, 2022-09, Vol.79 (5), p.935-950</ispartof><rights>2021 Informa UK Limited, trading as Taylor & Francis Group 2021</rights><rights>2021 Informa UK Limited, trading as Taylor & Francis Group</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c253t-7bb8034819fcc7e76f33dc4e64f64254b13777b291316ce637fe3a2b781c3d483</citedby><cites>FETCH-LOGICAL-c253t-7bb8034819fcc7e76f33dc4e64f64254b13777b291316ce637fe3a2b781c3d483</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Brammer, Hugh</creatorcontrib><title>Soil-environmental relationships on the Brahmaputra and Ganges floodplains in Bangladesh</title><title>International journal of environmental studies</title><description>The reconnaissance soil survey of Pakistan 1961-71 produced important new information on the environmental relationships of soils on the Brahmaputra and Ganges floodplains in East Pakistan (now Bangladesh) which provided a sound basis for agricultural land use planning in the country. The greater part of the territory was found to have been formed in sediments deposited by tributary and distributary rivers, not by the two major rivers themselves. Piedmont, river meander, estuarine and tidal floodplain landscapes of different ages were recognised, with intricate relief and soil patterns with associated local differences in land use and crop suitability. In all except current active floodplain and piedmont fan areas, seasonal flooding was found to be mainly by rainwater ponded on the floodplains by high seasonal flood levels in the major rivers flowing into the country. Therefore, the country's floodplains are not occupied, as is popularly believed, by sediments receiving annual increments of fertile alluvium; they are mainly occupied by soils developed to different degrees according to differences in sediment origin and landscape age, with profiles reflecting local differences in relief and drainage, and further changed by degradation through ferrolysis and by puddling of topsoils for rice cultivation.</description><subject>Agricultural land</subject><subject>Alluvial deposits</subject><subject>Alluvium</subject><subject>Bangladesh</subject><subject>Cultivation</subject><subject>Environmental science</subject><subject>Environmental studies</subject><subject>Estuaries</subject><subject>ferrolysis</subject><subject>Flood levels</subject><subject>Flooding</subject><subject>floodplain soil</subject><subject>Floodplains</subject><subject>Foothills</subject><subject>Grain cultivation</subject><subject>Land use</subject><subject>Land use management</subject><subject>Land use planning</subject><subject>Landscape</subject><subject>paddy soil</subject><subject>Puddling</subject><subject>Rain water</subject><subject>Rivers</subject><subject>Sediments</subject><subject>soil coatings</subject><subject>Soil surveys</subject><subject>Soils</subject><subject>Tidal 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soil</topic><topic>Floodplains</topic><topic>Foothills</topic><topic>Grain cultivation</topic><topic>Land use</topic><topic>Land use management</topic><topic>Land use planning</topic><topic>Landscape</topic><topic>paddy soil</topic><topic>Puddling</topic><topic>Rain water</topic><topic>Rivers</topic><topic>Sediments</topic><topic>soil coatings</topic><topic>Soil surveys</topic><topic>Soils</topic><topic>Tidal floods</topic><topic>toposequence</topic><topic>Topsoil</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Brammer, Hugh</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Toxicology Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research 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basis for agricultural land use planning in the country. The greater part of the territory was found to have been formed in sediments deposited by tributary and distributary rivers, not by the two major rivers themselves. Piedmont, river meander, estuarine and tidal floodplain landscapes of different ages were recognised, with intricate relief and soil patterns with associated local differences in land use and crop suitability. In all except current active floodplain and piedmont fan areas, seasonal flooding was found to be mainly by rainwater ponded on the floodplains by high seasonal flood levels in the major rivers flowing into the country. 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source | Taylor and Francis Social Sciences and Humanities Collection |
subjects | Agricultural land Alluvial deposits Alluvium Bangladesh Cultivation Environmental science Environmental studies Estuaries ferrolysis Flood levels Flooding floodplain soil Floodplains Foothills Grain cultivation Land use Land use management Land use planning Landscape paddy soil Puddling Rain water Rivers Sediments soil coatings Soil surveys Soils Tidal floods toposequence Topsoil |
title | Soil-environmental relationships on the Brahmaputra and Ganges floodplains in Bangladesh |
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