绿洲带地表水与地下水δD、δ~(18)O特征
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摘要
为探明新疆南部地区河流绿洲带地表水与地下水δD、δ~(18)O特征,于2016年7、8、11月和2017年7、8月在研究区进行δD、δ~(18)O样品采集。通过对河流绿洲带同一时期不同区域、不同时期同一区域的地表水与地下水δD、δ~(18)O在大气降水线上的分布特征分析发现:无论是同时期不同区域还是不同时期同一区域的地表水与地下水δD、δ~(18)O分布特征相似,分布于研究区冬、夏半年降水数据的交汇区域,并没有体现出取样月份的降水同位素特征,并且δD、δ~(18)O值均处于降水-融雪水-冰川水的δD、δ~(18)O值范围内,体现出其补给源存在多样性、变化性、累积性和滞后性的特点;同时,结合研究区实际情况分析表明,河流绿洲带水体的δD、δ~(18)O特征表现出其受到自然因素和人类活动的双重影响。
In order to perform a detailed investigation on the variation characteristics of δD and δ~(18)O in the oases in south Xinjiang,the samples of surface water and groundwater were collected in July,August and November 2016 and July and August 2017,respectively. After analyzing the characteristics of δD and δ~(18)O in surface water,groundwater and precipitation in different drainage basins in south Xinjiang in the same period,it was found that the distribution of δD and δ~(18)O in surface water and groundwater was similar. The isotopes were distributed at the intersection of precipitation data in winter and summer,and there was no a seasonal difference. The values were all in the range of δD and δ~(18)O in precipitation,snowmelt and glacier water. Which revealed the diversity,variation,accumulation and lagging characteristics of the recharge sources. Moreover,the characteristics of δD and δ~(18)O in surface water,groundwater and precipitation in the oases were jointly affected by both natural factors and human activities based on considering the actual situation of the study area.
In order to perform a detailed investigation on the variation characteristics of δD and δ~(18)O in the oases in south Xinjiang,the samples of surface water and groundwater were collected in July,August and November 2016 and July and August 2017,respectively. After analyzing the characteristics of δD and δ~(18)O in surface water,groundwater and precipitation in different drainage basins in south Xinjiang in the same period,it was found that the distribution of δD and δ~(18)O in surface water and groundwater was similar. The isotopes were distributed at the intersection of precipitation data in winter and summer,and there was no a seasonal difference. The values were all in the range of δD and δ~(18)O in precipitation,snowmelt and glacier water. Which revealed the diversity,variation,accumulation and lagging characteristics of the recharge sources. Moreover,the characteristics of δD and δ~(18)O in surface water,groundwater and precipitation in the oases were jointly affected by both natural factors and human activities based on considering the actual situation of the study area.
引文
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[21]姚一平,瓦哈甫·哈力克,伏吉芮.干旱区绿洲规模适宜度评价---以于田绿洲为例[J].湖南师范大学自然科学学报,2016,39(3):1-7.[Yao Yiping,Wahafu Halike,Fu Jirui.Study on the suitability evaluation of oasis scale in arid area:A case study of the Keriya Oasis[J].Journal of Natural Science of Hunan Normal University,2016,39(3):1-7.]
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[24]Mayr C,Lücke A,Stichler W,et al.Precipitation origin and evaporation of lakes in semi-arid patagonia(argentina)inferred from stable isotopes(δ18O,δ2H)[J].Journal of Hydrology,2007,334(1):53-63.
[25]王晓艳,卢爱刚,蒋缠文,等.渭南大气降水中氢氧同位素特征与水汽来源关系[J].干旱区资源与环境,2017,31(8):122-128.[Wang Xiaoyan,Lu Aigang,Jiang Chanwen,et al.Characteristics ofδD andδ18O in precipitation and the moisture origin in Weinan[J].Journal of Arid Land Resources and Environment,2017,31(8):122-128.]
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