Studying the Spatial Variations of Stable Isotopes (18O and 2H) in Precipitation and Groundwater Resources in Zagros Region
Commenced in January 2007
Frequency: Monthly
Edition: International
Paper Count: 33093
Studying the Spatial Variations of Stable Isotopes (18O and 2H) in Precipitation and Groundwater Resources in Zagros Region

Authors: Mojtaba Heydarizad

Abstract:

Zagros mountain range is a very important precipitation zone in Iran as it receives high average annual precipitation compared to other parts of this country. Although this region is important precipitation zone in semi-arid an arid country like Iran, accurate method to study water resources in this region has not been applied yet. In this study, stable isotope δ18O content of precipitation and groundwater resources showed spatial variations across Zagros region as southern parts of Zagros region showed more enriched isotope values compared to the northern parts. This is normal as southern Zagros region is much drier with higher air temperature and evaporation compared to northern parts. In addition, the spatial variations of stable isotope δ18O in precipitation in Zagros region have been simulated by the models which consider the altitude and latitude variations as input to simulate δ18O in precipitation.

Keywords: Groundwater, precipitation, simulation, stable isotopes, Zagros region.

Digital Object Identifier (DOI): doi.org/10.5281/zenodo.3593226

Procedia APA BibTeX Chicago EndNote Harvard JSON MLA RIS XML ISO 690 PDF Downloads 669

References:


[1] B. Alijani, “Iran climatology,” Tehran: Payam nour publication, 2000, pp. 250.
[2] U.S. Kumar, B. Kumar, S.P. Rai, S. Sharma, “Stable isotope ratios in precipitation and their relationship with meteorological conditions in the Kumaon Himalayas, India,” J. Hydrol. Vol. 391, 2010, pp. 1–8. https://doi.org/https://doi.org/10.1016/j.jhydrol.2010.06.019
[3] R. Gonfiantini, M.A. Roche, J.C. Olivry, J.C. Fontes, G.M. Zuppi, “The altitude effect on the isotopic composition of tropical rains,” Chem. Geol. Vol. 181, 2001, pp.147–167. https://doi.org/https://doi.org/ 10.1016/S0009-2541(01)00279-0
[4] H. Guan, C.T. Simmons, A.J. Love, “Orographic controls on rain water isotope distribution in the Mount Lofty Ranges of South Australia,” J. Hydrol. Vol.374, 2009, pp. 255–264. https://doi.org/https://doi.org/ 10.1016/j.jhydrol.2009.06.018
[5] E. Dotsika, S. Lykoudis, D. Poutoukis, “Spatial distribution of the isotopic composition of precipitation and spring water in Greece. Glob. Planet,” Change Vol. 71, 2009, pp. 141–149. https://doi.org/https://doi.org/ 10.1016/j.gloplacha.2009.10.007
[6] G. Vespasiano, C. Apollaro, R. Rosa, D. Muto, F. Larosa, S. Fiebig, J. Mulch, A. Marini, “The Small Spring Method (SSM) for the definition of stable isotope–elevation relationships in Northern Calabria (Southern Italy),” Appl. Geochemistry Vol. 63, 2015, pp.333–346. https://doi.org/https://doi.org/10.1016/j.apgeochem.2015.10.001
[7] D. Windhorst, T. Waltz, E. Timbe, H.-G. Frede, L. Breuer, “Impact of elevation and weather patterns on the isotopic composition of precipitation in a tropical montane rainforest,” Hydrol. Earth Syst. Sci. Vol. 17, 2015, pp. 409–419. https://doi.org/10.5194/hess-17-409-2013
[8] Bowen, G.J., Revenaugh, J., 2003. Interpolating the isotopic composition of modern meteoric precipitation. Water Resour. Res. 39.