NANOlab Center of Excellence literature database -- Query Results

“Chemical composition of river sediments from the Indian sub-continent”. Subramanian V, Van 't dack L, Van Grieken R, Chemical geology 48, 271 (1985). http://doi.org/10.1016/0009-2541(85)90052-X Abstract: River sediments from all of the major drainage basins (except the Indus) in the Indian sub-continent were collected and analysed by thin-film X-ray fluorescence technique (XRF) to determine their chemical composition. On the basis of analysis of more than 120 samples, average chemical compositions of river-borne sediments from the Indian sub-continent have been calculated. Also, average concentration values for sediments from each of the river basins, and the sub-continent average and the inter-basin differences are discussed in relation to weathering processes in the drainage basins. Comparisons have been made with the chemistry of sediments from the Bay of Bengal (which receives the bulk of sediments delivered by Indian rivers). Our observations are discussed in the light of average chemical composition of world-river sediments and the world surface rock exposed for continental weathering. Keywords: A1 Journal article; AXES (Antwerp X-ray Analysis, Electrochemistry and Speciation) DOI: 10.1016/0009-2541(85)90052-X Additional Links: UA library record; WoS full record; WoS citing articles show.php?record=7654
“Preliminary studies on the geochemistry of the Cauvery river basin”. Subramanian V, Van 't dack L, Van Grieken R, Proceedings of the Indian Academy of Sciences: earth and planetary sciences 94, 99 (1985). http://doi.org/10.1007/BF02871942 Abstract: Samples of water and sediments were collected over a three year period from the entire region of Cauvery river basin excluding the estuary. On the basis of our observations, we have calculated the average composition of the Cauvery river at several locations from the catchment to the river mouth, the downstream profile of sediment load, annual erosion rates, solute and sediment fluxes and have predicted on long term changes. The sediment chemistry was determined by x-ray fluorescence (xrf) technique, and calculated mean compositions of the Cauvery and its tributary bed and the suspended sediment were compared to those of world average river sediments. Downstream profiles of some of the elements appear to be controlled by size and mineralogical characteristics besides local factors specific to the location of the samples. Interelemental relationships indicated good correlation among the transition elements indicating their co-genetic behaviour within the drainage basin. Keywords: A1 Journal article; AXES (Antwerp X-ray Analysis, Electrochemistry and Speciation) DOI: 10.1007/BF02871942 Additional Links: UA library record; WoS full record; WoS citing articles show.php?record=8410

Abstract: River sediments from all of the major drainage basins (except the Indus) in the Indian sub-continent were collected and analysed by thin-film X-ray fluorescence technique (XRF) to determine their chemical composition. On the basis of analysis of more than 120 samples, average chemical compositions of river-borne sediments from the Indian sub-continent have been calculated. Also, average concentration values for sediments from each of the river basins, and the sub-continent average and the inter-basin differences are discussed in relation to weathering processes in the drainage basins. Comparisons have been made with the chemistry of sediments from the Bay of Bengal (which receives the bulk of sediments delivered by Indian rivers). Our observations are discussed in the light of average chemical composition of world-river sediments and the world surface rock exposed for continental weathering.

Abstract: Samples of water and sediments were collected over a three year period from the entire region of Cauvery river basin excluding the estuary. On the basis of our observations, we have calculated the average composition of the Cauvery river at several locations from the catchment to the river mouth, the downstream profile of sediment load, annual erosion rates, solute and sediment fluxes and have predicted on long term changes. The sediment chemistry was determined by x-ray fluorescence (xrf) technique, and calculated mean compositions of the Cauvery and its tributary bed and the suspended sediment were compared to those of world average river sediments. Downstream profiles of some of the elements appear to be controlled by size and mineralogical characteristics besides local factors specific to the location of the samples. Interelemental relationships indicated good correlation among the transition elements indicating their co-genetic behaviour within the drainage basin.

Keywords: A1 Journal article; AXES (Antwerp X-ray Analysis, Electrochemistry and Speciation)

DOI: 10.1007/BF02871942

Additional Links: UA library record; WoS full record; WoS citing articles

show.php?record=8410