05343nam 2201345z- 450 991055729050332120231214133140.0(CKB)5400000000041134(oapen)https://directory.doabooks.org/handle/20.500.12854/69194(EXLCZ)99540000000004113420202105d2020 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierUse of Water Stable Isotopes in Hydrological ProcessBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20201 electronic resource (296 p.)3-03943-266-4 3-03943-267-2 Stable and radioactive isotopes in water are powerful tools in the tracking of the path of water molecules through the whole water cycle. In the last decade, a considerable number of studies have been published on the use of water isotopes, and their number is ever-growing. The main reason is the development of new measurement techniques (i.e., laser absorption spectroscopy) that allow measurements of stable isotope ratios at ever-higher resolutions. Therefore, this compilation of papers has been published to address the current state-of-the-art water isotope methods, applications, and interpretations of hydrological processes, and to contribute to the rapidly growing repository of isotope data, which is important for future water resource management. We are pleased to present here a book with new findings in thirteen original research papers and one review paper issued in the Water MDPI Special Issue (SI) “Use of Water Isotopes in Hydrological Processes”. The authors report the use of water isotopes in hydrological processes worldwide, including studies at both local and regional scales related to either precipitation dynamics or to different applications of water isotopes in combination with other hydrochemical parameters in investigations of surface water, snowmelt, soil water, groundwater and xylem water to identify the hydrological and geochemical processes.Research & information: generalbicsscprecipitationstable isotope ratioslocal meteoric water lineamount-weighted meanlinear regressionconfidenceprediction and generalized intervalsstable isotopes D and 18Omoisture sourcetemperature effectprecipitation amount effectregionalizationChinaoxygen isotopessulfur isotopesisotopic composition of waterbacterial sulfate reductionsulfide oxidationatmospheric sulfatepeatlandunconfined aquifermineralization of organic matterisotopic techniqueswater isotopic signature3H- and 14C-datingsaltwater intrusionRed River’s deltaVietnamSutri DhakaChandra BasinWestern Himalayahydrograph separationstable water isotopespecific ablationstable isotopesHYSPLIT modelMWL validationkarstic springsspatial variationsNaqu River basinQinghai–Tibet Plateaustable water isotopeshydrogenoxygensoil waterfine root systemgroundwaterisotope hydrologystable nitrate isotopesZagrebCroatia2H/1H and 18O/16Odeuterium excessδ18O–temperature relationtritiumself-organizing mapradonmajor ionsalluvial fanpaddy rice fielddeuterium and oxygen-18hydrogeological conceptual modelalluvial aquiferVaraždin areaδ2Hinverse modelingvadose zonesensitivity analysissoil hydraulic parameters estimationgroundwater recharged-excesselevation effectaltitude effectcontinental effectSloveniaHungarywater cyclemeasurement traceabilityprecipitation (rain and snow)surface waterwater managementnetworks and data basesstatistical evaluationResearch & information: generalVreča Polonaedt1296150Kern ZoltánedtVreča PolonaothKern ZoltánothBOOK9910557290503321Use of Water Stable Isotopes in Hydrological Process3023811UNINA