Abstract
Stable hydrogen (δD) and oxygen (δ18O) isotope ratios of the headwaters of the Indus and its tributaries, surface ice in glaciers, saline and fresh water lakes and thermal springs in the Himalayan and Trans-Himalayan (Kashmir) region are reported. The δ5D-δ18 relationship for the river samples shows a slope of 9.12 +-0.29 which agrees well with the estimate of 8.99 ±0.33 based on a simple Rayleigh fractionation model. The unique signature of a higher deuterium excess (d) of the ‘Western Disturbance’ is preserved in these samples. An altitude effect of -0.9 per mil/km is observed in the δ18O of Indus waters. At a lower altitude (Beas) the altitude effect is almost double, indicating that the altitude effect decreases with elevation in this region.
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Bartarya S K, Bhattacharya S K, Ramesh R and Somayajulu B L K 1995 δ18O and δD systematics in the surficial waters of the Gaula river catchment area, Kumaun Himalaya, India;J. Hydrology 167 369–379
Epstein S and Mayeda T 1953 Variation of δ18O content in waters from natural sources;Geochim. Cosmochim. Acta 4 213–224
Friedman I 1953 Deuterium content of natural waters and other substances;Geochim. Cosmochim. Acta 4 89–103
Gat J R and Carmi I 1970 Evolution of the isotopic composition of atmospheric waters in the Mediterranean sea area;J. Geophys Res,75 3039–3048
Gat J R 1981 InStable Isotope Hydrology (eds.) J R Gat and R Gonfiantini, IAEA Tech. Rep. Ser.210 7–19
Giggenbach W F, Gonfiantini R, Jangi B L and Truesdell A H 1983 Isotopic and chemical composition of Partabi Valley geothermal discharges, north-west Himalaya, India;Geothermics 12 (2/3) 199–222
Gonfiantini R, Gallo G, Payne B R and Taylor C B 1976 Environmental isotopes and hydrochemistry in ground water of Gran Canaria. In:Interpretation of environmental isotope and hydrochemical data in ground water hydrology pp 159–170 Vienna: IAEA
Gonfiantini R 1981 In:Stable Isotope Hydrology (eds) J R Gat and R Gonfiantini, IAEA Tech Rep Ser210 35–85
Grabczak J and Kotarba M 1985 Isotopic composition of the thermal waters in the central part of the Nepal Himalayas;Geothermics 14 (4) 567–575
Jouzel J and Merlivat L 1984 Deuterium and oxygen 18 in precipitation: Modelling of the isotopic effect during snow formation;J. Geophys. Res. 89 11749–11757
Majoube M 1971 Fractionnement en oxygene 18 et en deuterium entre l’eau et sa vapeur;J. Chim. Phys. 10 1423–1436
Mayewski P A and Lyons W B 1983 Chemical composition of a high altitude fresh snow fall in the Ladakh Himalayas;Geophys. Res. Lett. 10 (1) 105–108
Navada S V, Nair A R, Sharma S and Kulkami U P 1985 Geochemical and Isotope studies of the geothermal areas of central and northern India;Isotope and geochemical techniques applied to geothermal investigations. (IAEA-TECDOC-)788 63–82
Niewodniczanski J, Grabczak J, Baranski L and Rzepka J 1981 The altitude effect on the isotopic composition of snow in higher mountains;J Glaciol 27 99–112
Raina A N 1977Geography of Jammu and Kashmir (New Delhi: National Book Trust) 271 p
Ramesh R and Sarin M M 1992 Stable isotope study of the Ganges (Ganga) river system;J. Hydrol. 139 49–62
Rozanski K, Arguas L A and Gonfiantini R 1993 Isotopic patterns in modern global precipitation; In:Climate change in continental isotopic indicators geophys mon 78 Am. Geophys. Union 1–36
Williamson J H 1968 Least square fitting of a straight line;Can. J. Phys. 46 1845–1847
World Weather Records 1967 Washington DC: U.S. Dept. of Commerce4 372
Yurtsever Y and Gat J R 1981 In:Stable isotope hydrology (eds) J R Gat and R Gonfiantini (IAEA Tech Rep Ser)210 103–142
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Pande, K., Padia, J.T., Ramesh, R. et al. Stable isotope systematics of surface water bodies in the Himalayan and Trans-Himalayan (Kashmir) region. J Earth Syst Sci 109, 109–115 (2000). https://doi.org/10.1007/BF02719154
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DOI: https://doi.org/10.1007/BF02719154