{"title":"New Approach for the Analysis of Isotopic Composition in Precipitation Globally","authors":"Bp Singh","doi":"10.4172/2157-7587.1000225","DOIUrl":null,"url":null,"abstract":"Isotopic composition of hydrogen and oxygen of water in precipitation is important tool to analyze the water in hydrological cycle. A new method has been suggested by Singh [7] plotting slope versus intercept of Local Meteoric Water Line (LMWL) to find the original isotopic composition in precipitation as injected tracer globally. Singh [8-10] has applied these concepts to analyze the isotopic composition in precipitation in different catchment areas of river and different seasons, precipitation falling at different altitudes in a region or a place and across the continent. These studies are extended for the (a) study of changing intercept but keeping the same slope as attributed to changed conditions as the source of atmospheric moisture. The experimental data as available of two transect from Amazon to Altiplano in South America are analyzed. The results are presented assigning two components, one due to Rayleigh adiabatic condensation process rainfall and second recycled water vapour by evotranspiration. The details of the analysis are given and the results clearly indicate these two components, are discussed in detail. (b) Study of higher intercept due to Mediterranean Meteoric Water Line (MMWL), Israel samples from various inputs on mountains, coastal area, caves and valley to ascertain the precipitation is from the same source. (c) Study of LMWL across the country (India) for four different regions to obtain the LMWL of the regions by the method of Singh [7] obtained the original isotopic composition of water in all the four regions thereby get the Global Meteoric Water Line (GMWL).","PeriodicalId":17605,"journal":{"name":"Journal of Waste Water Treatment and Analysis","volume":"50 1","pages":"1-7"},"PeriodicalIF":0.0000,"publicationDate":"2015-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Waste Water Treatment and Analysis","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4172/2157-7587.1000225","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
Isotopic composition of hydrogen and oxygen of water in precipitation is important tool to analyze the water in hydrological cycle. A new method has been suggested by Singh [7] plotting slope versus intercept of Local Meteoric Water Line (LMWL) to find the original isotopic composition in precipitation as injected tracer globally. Singh [8-10] has applied these concepts to analyze the isotopic composition in precipitation in different catchment areas of river and different seasons, precipitation falling at different altitudes in a region or a place and across the continent. These studies are extended for the (a) study of changing intercept but keeping the same slope as attributed to changed conditions as the source of atmospheric moisture. The experimental data as available of two transect from Amazon to Altiplano in South America are analyzed. The results are presented assigning two components, one due to Rayleigh adiabatic condensation process rainfall and second recycled water vapour by evotranspiration. The details of the analysis are given and the results clearly indicate these two components, are discussed in detail. (b) Study of higher intercept due to Mediterranean Meteoric Water Line (MMWL), Israel samples from various inputs on mountains, coastal area, caves and valley to ascertain the precipitation is from the same source. (c) Study of LMWL across the country (India) for four different regions to obtain the LMWL of the regions by the method of Singh [7] obtained the original isotopic composition of water in all the four regions thereby get the Global Meteoric Water Line (GMWL).
降水中水的氢氧同位素组成是分析水循环过程中水的重要工具。Singh[7]提出了一种新的方法,通过绘制当地大气水线(Local Meteoric Water Line, LMWL)的斜率与截距来寻找全球注入示踪剂降水中的原始同位素组成。Singh[8-10]应用这些概念分析了河流不同集水区和不同季节、一个地区或一个地方不同海拔和整个大陆的降水中的同位素组成。这些研究被扩展为(a)由于大气湿度来源的变化而导致的截距变化但保持相同斜率的研究。对南美洲亚马孙至高原两个样带的实验数据进行了分析。结果提出了两个组成部分,一个是由于瑞利绝热凝结过程的降雨,第二个是由蒸发蒸腾的再循环水蒸气。给出了详细的分析结果,并对这两个组成部分进行了详细的讨论。(b)研究由于地中海大气水线(MMWL)造成的较高截距,以色列从山区、沿海地区、洞穴和山谷的不同输入取样,以确定降水来自同一来源。(c)研究全国(印度)四个不同地区的LMWL,通过Singh[7]的方法获得该地区的LMWL,得到所有四个地区的水的原始同位素组成,从而得到全球大气水线(GMWL)。