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2. Beijing Hydrological Center, Beijing 100089, China, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=Rqjsu/MOWLlr7T1zGVjqIQ==, pdfFileSize=3894470, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1242135257835713234, articleId=1242135254861951689, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=北疆大气降水水汽源识别及其对地下水补给的指示意义, columnId=1146540929516700224, journalTitle=科技导报, columnName=研究论文, runingTitle=null, highlight=null, articleAbstract=大气降水是水循环的输入项,其同位素特征是示踪水汽来源及运动路径的有效工具。利用北疆4个大气降水观测站的同位素数据,结合HYSPLIT模式,重点分析了北疆大气降水同位素特征。区域大气降水线方程δ D=7.3δ 18 O+3.5,反映了新疆独特的干旱气候环境。受不同降水水汽来源影响,天山及阿勒泰2个地区降水同位素特征表现不同。天山地区受西风带水汽季节性漂移的影响,氘盈余夏季低冬季高,成“V”型;阿勒泰地区常年受北冰洋水汽影响,氘盈余年内变幅不明显。尽管δ 18 O均表现为夏季富集、冬季贫化,但多年均值差异明显,该差异也使得利用同位素确定地下水补给来源成为可能。准东盆地东天山附近地下水主要受到来自东天山的大气降水补给,而北侧自流区地下水同位素相对贫化,与阿勒泰站大气降水同位素及氘盈余特征相似,结合地形、水文地质条件等特征,认为该区主要受克拉美丽山大气降水补给。, authors=李捷1 , 庞忠和1 , 古丽波斯坦·吐逊江1 , 孔彦龙1 , 黄天明1 , 白国营2 , 赵泓漪2 , 周东2 , 杨忠山2 , authorsList=李捷, 庞忠和, 古丽波斯坦·吐逊江, 孔彦龙, 黄天明, 白国营, 赵泓漪, 周东, 杨忠山, authorCompany=1. 中国科学院地质与地球物理研究所, 页岩气与地质工程重点实验室, 北京 100029;
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科技导报
| 研究论文 2016, 34(18): 118-124
北疆大气降水水汽源识别及其对地下水补给的指示意义
全屏
李捷1 , 庞忠和1 , 古丽波斯坦·吐逊江1 , 孔彦龙1 , 黄天明1 , 白国营2 , 赵泓漪2 , 周东2 , 杨忠山2
作者信息
1. 中国科学院地质与地球物理研究所, 页岩气与地质工程重点实验室, 北京 100029;
2. 北京市水文总站, 北京 100089
通讯作者:
庞忠和(通信作者),教授,研究方向为水循环与水岩相互作用,电子信箱:z.pang@mail.iggcas.ac.cn
Identification of moisture sources in Junggar Basin and its implication for groundwater recharge
Affiliations
出版时间: 2016-09-28
doi: 10.3981/j.issn.1000-7857.2016.18.015
文章导航
大气降水是水循环的输入项,其同位素特征是示踪水汽来源及运动路径的有效工具。利用北疆4个大气降水观测站的同位素数据,结合HYSPLIT模式,重点分析了北疆大气降水同位素特征。区域大气降水线方程δ D=7.3δ 18 O+3.5,反映了新疆独特的干旱气候环境。受不同降水水汽来源影响,天山及阿勒泰2个地区降水同位素特征表现不同。天山地区受西风带水汽季节性漂移的影响,氘盈余夏季低冬季高,成“V”型;阿勒泰地区常年受北冰洋水汽影响,氘盈余年内变幅不明显。尽管δ 18 O均表现为夏季富集、冬季贫化,但多年均值差异明显,该差异也使得利用同位素确定地下水补给来源成为可能。准东盆地东天山附近地下水主要受到来自东天山的大气降水补给,而北侧自流区地下水同位素相对贫化,与阿勒泰站大气降水同位素及氘盈余特征相似,结合地形、水文地质条件等特征,认为该区主要受克拉美丽山大气降水补给。
大气降水
/
稳定同位素
/
氘盈余
/
水汽来源
/
北疆
/
地下水补给
Precipitation is the input of the water cycle, and stable isotopes of precipitation (18O and 2 H) are powerful tools in tracing moisture sources and trajectories. In this paper, the characteristics of stable isotopes and deuterium excess in the precipitation are analyzed in the North Xinjiang based on observation data of four precipitation stations and HYSPLIT model. The local meteoric water line (LMWL) is established as δ D=7.3δ 18 O+3.5, indicating the specific regional meteorological conditions. The Tianshan area and Altay area showed different isotopic characteristics due to different moisture sources. The monthly deuterium values in Tianshan area are low in summer and high in winter, which can be attributed to the seasonal drift of the westerlies. The monthly deuterium values in Altay area are constant due to the effect of arctic air mass. Although the monthly δ 18 O values in both areas are high in summer and low in winter, the amount-weighted averages are diverse, which makes it possible for identifying groundwater recharge areas. The intersection point of the evaporation line near Kelameili Mountain and LMWL has similar values of stable isotopes to the precipitation from Altay station, indicating that groundwater recharge from Kelameili Mountain. Groundwaters near East Tianshan Mountain have similar δ 18 O values, similar to the precipitation from Urumqi station, which suggesting groundwater in this area is recharged from East Tianshan Mountain.
precipitation
/
stable isotopes
/
deuterium excess
/
moisture sources
/
North Xinjiang
/
groundwater recharge
李捷, 庞忠和, 古丽波斯坦·吐逊江, 孔彦龙, 黄天明, 白国营, 赵泓漪, 周东, 杨忠山.
北疆大气降水水汽源识别及其对地下水补给的指示意义.
科技导报,
2016
, 34
(18)
: 118
-124
.
DOI: 10.3981/j.issn.1000-7857.2016.18.015
LI Jie, PANG Zhonghe, TURSUN Gulbostan, KONG Yanlong, HUANG Tianming, BAI Guoying, ZHAO Hongyi, ZHOU Dong, YANG Zhongshan.
Identification of moisture sources in Junggar Basin and its implication for groundwater recharge[J].
Science & Technology Review ,
2016
, 34
(18)
: 118
-124
.
DOI: 10.3981/j.issn.1000-7857.2016.18.015
2016年第34卷第18期
PDF下载
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引用本文
BibTeX
文章信息
doi: 10.3981/j.issn.1000-7857.2016.18.015
接收时间:2015-11-24
首发时间:2016-10-21
出版时间:2016-09-28
收稿日期:2015-11-24
修回日期:2016-03-18
通讯作者:
庞忠和(通信作者),教授,研究方向为水循环与水岩相互作用,电子信箱:z.pang@mail.iggcas.ac.cn
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2016.18.015
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2种不同金属材料的力学参数
科 Family 属数 Number of genus 种数 Number of species 占总种数比例 Percentage of total species (%) 属 Genus 种数 Number of species 占总种数比例 Percentage of total species (%) 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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