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| 1 | 西北干旱区降水中氢氧同位素研究进展显示文摘借助近年来的相关研究文献对中国西北干旱区降水中氢氧同位素特征和相关科学问题进行了梳理和总结,主要结果:①西北干旱区降水稳定同位素呈现出显著的季节性变化,夏半年高,冬半年低,充分体现了同位素分布的温度效应;从空间上看,同位素低值区分布在天山等山地,盆地为高值区。②温度是西北干旱区大气降水同位素组成的主要控制因素;事件降水尺度上部分区域夏季存在降水量效应;地理因素及水汽来源等对大气降水同位素的分布有区域性差异。③西北干旱区区域大气降水线斜率和截距均较低,整体显示出干旱的气候特点,但内部地域差异性显著。④降水中过量氘值变化幅度大,体现了西北干旱区水汽来源复杂、降水形成时环境要素差异性大的特点;过量氘具有冬高夏低的特点,但由于夏季存在强烈蒸发,部分站点也呈现出冬低夏高的特点。⑤西北干旱区降水主要水汽来源为西风带,也会受到季风和极地气团的影响。 | 曾帝 吴锦奎 李洪源 赵求东 刘世伟 秦甲 | 2020 | 干旱区研究2020，37，4： | 20 |
| 2 | 乌鞘岭南、北坡降水稳定同位素特征及水汽来源对比显示文摘为了揭示季风边缘区降水中稳定同位素特征及水汽来源,利用2016年10月至2017年10月采集的97个降水样品,采用相关分析和HYSPLIT模型,对乌鞘岭南、北坡降水稳定同位素的特征、大气水线方程、温度和降水量效应、水汽来源进行了对比分析.结果表明,南坡大气降水线的斜率与截距低于全球大气水线(GMWL)和北坡大气降水线;南、北坡的同位素温度效应和季节效应明显,但北坡的温度效应比南坡更为明显;除北坡夏季和南坡降水量小于5 mm时降水稳定同位素表现出微弱的降水量效应,南、北坡其它季节或其它降水量级均无明显的降水量效应;来自西北和北方的水汽占90%以上,北坡受季风水汽影响极少,南坡夏季会受到东南季风影响,局地水汽再循环对乌鞘岭南、北坡水汽也有贡献.本研究可提高对高寒山区降水同位素演化的认知,为寒旱区同位素水文学的进一步研究奠定基础. | 徐秀婷 贾文雄 朱国锋 马兴刚 张昱 袁瑞丰 张志远 石阳 | 2020 | 环境科学2020，41，1： | 12 |
| 3 | 北山地区大气降水中水化学及稳定同位素特征显示文摘为揭示甘肃北山地区大气降水的水化学及同位素特征,利用2012~2019年度采集的97件大气降水样品,采用相关性分析,富集因子,气团后向轨迹分析等多种方法对北山地区稳定同位素变化特征及其影响因素,降水中主要离子变化特征,不同离子来源及贡献,水汽来源进行了分析.结果表明,北山地区区域降水线的斜率与截距均高于张掖地区大气降水线;该区降水中稳定同位素比率明显受季节性,温度和高程效应的影响,在年尺度下,降雨量效应不明显;该区降水中氘盈余变化较大,雨季降水中氘盈余显著小于旱季降水中氘盈余值;北山地区大气降水的水化学型主要为HCO3·SO4-Ca和HCO3-Ca型,降水中离子浓度具有明显的季节性变化,降雨量的增加对离子浓度具有一定的稀释作用;Na^+受海源和陆源物质的双重影响;绝大部分的Ca^2+,K^+,HCO3^-和部分Mg^2+来源于陆源,SO4^2-与NO3^-的主要来自于人类活动输入;区内冬夏季水汽来源基本一致,来源于西北方向的季风源是北山地区最主要的水汽来源.研究成果可为我国高放废物地质处置库选址和性能评价以及未来地下处置库建设提供依据,也有助于丰富西北干旱区的水文循环过程研究. | 李杰彪 苏锐 周志超 郭永海 | 2020 | 中国环境科学2020，40，12： | 4 |
| 4 | Isotopic evidence for the moisture origin and influencing factors at Urumqi Glacier No.1 in upstream Urumqi River Basin, eastern Tianshan Mountains显示文摘The stable isotope has been extensively applied as an effective tracer especially in precipitation. In glacierized area of arid northwest China, temperature is widely considered to be a major factor affecting isotopes in precipitation, while the influences of precipitation amount, relative humidity and other meteorological parameters are still not clear. Based on analyses on stable isotope values of water samples and NCEP/NCAR(National Centers of Environmental Prediction/National Center for Atmospheric Research, USA) re-analysis data, the moisture source and characteristics of isotopes in the precipitation, meltwater and river water isotopes at Urumqi Glacier No.1 of the upstream Urumqi River Basin, eastern Tianshan Mountains from spring to autumn during four years(from 2008 to 2011) was studied. Results indicated that meltwater are the main source of water for the upper Urumqi River. Seasonal variation of δ18 O in precipitation demonstrated that δ18 O was more enriched in summer and depleted in spring and autumn. Temperature was positively correlated with isotopes, while precipitation amount and relative humidity was negatively correlated with isotopes. The water vapor was affected by westerly air mass and regional water vapor cycle. Meanwhile, back trajectory clustering analyses showed that the moisture mainly from Europe and central Asia. The moisture was more likely to be locally sourced with the ratio was 46.8%~52.1%. | SONG Meng-yuan LI Zhong-qin XIA Dun-sheng JIN Shuang ZHANG Xin | 2019 | Journal of Mountain Science2019，16，8： | 2 |
| 5 | Contribution of Hydrogeochemical and Isotopic Tools to the Management of Upper and Middle Cheliff Aquifers显示文摘In the alluvial aquifers of Upper and Middle Cheliff(North-West Algeria), the groundwater quality is deteriorating. The objective of this study was to characterize the physical and chemical properties of these aquifers;and to evaluate the groundwater quality and its appropriateness for drinking and agricultural use. An investigation was carried out by estimating of the physiochemical parameters(Ca^2+, Mg^2+, Na^+, K^+, Cl^-, SO4^2-, HCO3^-, NO3^-, Br^- and TDS) to identify the chemical characteristics of groundwater. Morever, the isotopic composition was examined to identify the sources of recharge of these aquifers. The groundwater geochemistry for the high water level(May, 2012 and June, 2017) and low water level(November, 2012 and October, 2017) was studied. Accordingly, water samples from 39 water sampling points were collected(October, 2017 and June, 2018), for the purpose of analyzing stable isotopes(18O, 2H). The results show that the groundwater is mainly characterized by Ca-Cl and Na-Cl type. The chemical quality of the water is from fair to poor with the presence of nitrates used in agricultural and urban discharge. Also, the Br/Cl ratio gives indications on the origin of the salinity. This salinity is due to the leaching of chlorinated fertilizers, the dissolution of evaporite deposits and the rise of deep salty water by the fault of Chellif. While, the diagram of δ2H=f(δ18O) indicates that the origin of the recharge of these aquifers is the Atlantic and Mediterranean oceanic meteoric rainwater. | Madene Elaid Meddi Hind Boufekane Abdelmadjid Meddi Mohamed | 2020 | Journal of Earth Science2020，31，5： | 1 |
| 6 | 高分辨氢同位素质谱仪的研制与应用显示文摘基于聚变核材料科研和生产、高温气冷堆产氚、氚放射性环境监测的需要设计了一套用于氢同位素分析的高分辨氢同位素质谱仪(HR-IRMS),通过简单易操作的压强法配气系统,建立了氢氘氚配气装置。所研制的HR-IRMS仪器分辨率达2210,测量精密度达0.02%,相对原子质量范围为1~150。比对分析表明,其具有良好的运行稳定性和测定结果准确性,可实现氢同位素直接分析。 | 石磊 侯艳丽 | 2021 | 原子能科学技术2021，55，3： | 0 |
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