Early Career: Acquisition of an Isotopic Liquid-Water Analyzer for Hydrology and Earth Science Research and Education at Syracuse University

建议摘要：液态水同位素分析仪是便携式用户友好的仪器，依靠近红外吸收光谱法来确定水样的同位素组成。 这项技术是商业上可用的，最近的进展使仪器成为传统稳定同位素比质谱仪的替代品。 该仪器只需要少量的样品，有限的样品预处理，并允许高精度的快速分析，因此为需要水同位素分析的各种研究项目打开了大门。 该补助金支持三名专门从事水文学，构造地貌学和水地球化学领域的早期职业科学家。 该仪器将支持的研究包括：确定水的同位素特征，以调查降雨和土壤水的来源;确定水的同位素组成在穿过水圈并最终纳入岩石记录时如何演变;分析海洋沉积物中的孔隙水，以跟踪南极峡湾的冰川融化事件;以及利用伊凯特矿物中的水来重建千年时间间隔的海水成分。 水（H2O）可以通过分析H和O的同位素来表征。 这两种元素的同位素组成包含了关于水的来源和影响水的气候过程的性质的大量信息。 例如，氧和氢同位素被用来确定有多少雨水来自海洋蒸发，以及水从海洋到地面并流入河流或地下水的距离。 该仪器将使早期的职业研究人员能够快速，准确和经济地分析从溪流，地下水和海洋中收集的样品的水同位素组成。 获得这一仪器将有助于开展的研究项目包括：确定地下沃茨、土壤水和溪流水的来源，了解岩石记录中水的同位素组成是如何保存的，确定冰川融化对南极海洋的水贡献的特征，以及通过分析矿物中的水来确定古代海水的组成。 这些应用对地球有影响吗？水循环、地球地形的演变以及气候变化对海水成分的影响。

Proposal Abstract:Liquid water isotope analyzers are portable user-friendly instruments that rely on near-infrared adsorption spectroscopy to determine the isotopic composition of water samples. This technology is commercially available and recent advances have made the instruments an alternative to traditional stable isotope ratio mass spectrometers. The instrument requires only a small sample volume, limited sample pre-processing, and allows for rapid analyses with high precision, therefore opening the door for a variety of research projects that require water isotope analyses. This grant supports three early career scientists that specialize in the fields of hydrology, tectonic geomorphology and aqueous geochemisty. The research that will be supported by this instrument includes characterization of water isotopes to investigate the sources of rainfall and soil water; the characterization of how water's isotopic composition evolves as it moves through the hydrosphere and is eventually incorporated into the rock record; the analyses of pore water in marine sediments to track glacial melting events in Antarctica fjords; and the use of water in ikaite minerals to reconstruct the composition of seawater on thousand-year time intervals. Water (H2O) can be characterized by analyzing the isotopes of both H and O. The isotopic composition of these two elements contains vast information on the sources of the water and the nature of the climatic processes that have affected the water. For instance, oxygen and hydrogen isotopes are used to determine how much rainwater originated from ocean evaporation and how far the water has traveled from the ocean to where it fell on the ground and feeds streams or groundwaters. The instrument funded though this grant will allow early career researchers to rapidly, precisely and economically analyze the water isotope composition of samples collected from streams, groundwaters, and the ocean. Research projects that will be facilitated by acquisition of this instrument include determining the sources of ground waters, soil water and stream water, learning how the isotopic composition of water is preserved in the rock record, characterizing the water contribution to the Antarctic ocean from melting of glaciers, and determining the composition of ancient sea water through analyses of water trapped in minerals. These applications have implications for the Earth?s water cycle, evolution of the Earth's topography, as well as the effects of climatic change on the ocean water composition.