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Sources and Ages of Ground Water in Unconfined and Confined Aquifers Beneath theU.S. High Plains

机译：美国境内无侧限和承压含水层地下水的来源和年龄。高原

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The objectives of the research are to (1) determine whether age and source ofunconfined and confined ground waters are the same beneath the southern, central, and northern High Plains, (2) determine whether confined ground water is derived from vertical leakage or from lateral inflow from an outcropping recharge area before hydrologic divides are formed, (3) evaluate whether geomorphologic or climatic change during the Quaternary accounts for the isotopically distinct ground water in confined aquifers, and (4) consider the implications of variations in isotopic composition of ground water for Quaternary paleoclimatology of the continental interior.

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作者
Dutton, A. R.;
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年度 1993
页码 1-52
总页数 52
原文格式 PDF
正文语种 eng
中图分类工业技术;
关键词
Aquifers; Ground water; Age estimation; Water sources; Water chemistry; Chemicalanalysis; Meteoric water; Chemical properties; Hydrogeology; Isotopes; Carbon 14; Carbon 13; Chlorine 36; Hydrogen 3; Oxygen 18;

机译：含水层;地下水;年龄估算;水源;水化学;化学分析;大气降水;化学特性;水文地质;同位素;碳14;碳13;氯36;氢3;氧18;

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Sources and Ages of Ground Water in Unconfined and Confined Aquifers Beneath theU.S. High Plains

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