Collaborative Research: Testing Potential of Paired Lakes on the NE Tibetan Plateau for Studying Interaction Between Hydrochemical Evolution and Environmental Change

湖水化学成分的演变取决于流入的水和随后的蒸发浓度以及矿物质的沉淀。在封闭盆地湖泊中，蒸发浓度主要由区域气候变化导致的干旱变化决定。然而，湖泊水与地下水化学、湖泊沉积物地球化学和环境变化之间的相互作用尚未在短期或长期尺度上进行研究，也很少采用多学科方法。智力上的优点。这项试点研究旨在调查干旱的青藏高原东北部成对的化学对比湖泊（淡水湖和咸水湖）。这些湖泊可能是研究水同位素和元素演化以及环境变化和湖泊地球化学过程相互作用的理想场所。拟议研究的总体目标是了解水化学演化及其在不同时间尺度上如何与各种环境控制相互作用。在东亚季风北部边界附近的气候敏感地区进行此类研究的额外好处是提高我们读取该地区湖泊沉积物记录的能力，以更好地了解过去的环境变化。我们建议采用多学科方法来研究区域和流域尺度、这两个湖泊的现代过程、来自矿物学和自生矿物和生物矿物的化学和同位素组成的溶质和水通量的历史、介形类的物种组合以及来自花粉、植物大化石和环境磁等景观过程记录的气候和环境变化的历史。该项目的结果将为理解湖泊的路径和机制提供见解。溶质演化和水通量以及它们如何影响过去环境变化的沉积记录。这是第一项采用多学科方法来解决中亚湖泊与气候相互作用的研究。该项目的一个关键特点是使用成对的湖泊学和化学对比湖泊，以揭示湖泊水文和水化学过程与环境（和气候）变化之间的相互作用。对稀水湖（克卢克湖）与咸水湖（托森湖）的现代响应的研究将使古水化学的全面而稳健的重建成为可能。此外，拟议研究中使用的多种技术将提供区域气候变化、流域稳定性和植被以及湖泊化学变化的独立记录。这些记录的整合将使我们能够关注不同时间尺度（从当今到间冰期循环）这些过程之间复杂的相互作用和反馈。更广泛的影响。我们的跨学科研究将增进对不同气候条件下这些系统复杂相互作用的理解。了解湖泊和流域对过去气候变化的反应将有助于我们预测气候（尤其是季风）变化和变率对环境造成的后果。我们使用成对的淡水湖和咸水湖对比水化学的方法并不常用，但我们相信这是一种非常有启发性的方法，具有巨大的回报。了解水文动态将有利于中国这个偏远干旱地区的人们适应未来潜在的气候和水文循环变化。研究结果将与半干旱北部大平原湖泊对气候和水文变化的响应进行比较，并与国家地质调查局和水利委员会共享。一旦通过试点阶段，研究生和本科生将更充分地参与该项目，并将从与国际多学科研究团队的互动中受益。该项目将促进合作，特别是与我们的中国同事的合作，他们在国际科技领域的影响力正在不断增强。

The evolution of the chemical composition of lake waters is determined by the inflow waters andsubsequent evaporative concentration and the precipitation of minerals. In closed-basin lakes, evaporativeconcentration is mostly determined by changes in aridity, as a result of regional climate change. However,the interactions among lake water and groundwater chemistries, lake sediment geochemistry, andenvironmental change have not been studied over short or long time scales, and seldom usingmultidisciplinary approach.Intellectual merits. This pilot study is to investigate paired chemically-contrasting lakes (fresh andsaline) in the arid northeastern Tibetan Plateau. These lakes are likely to be ideal sites for the study ofwater isotopic and elemental evolution, and the interactions of environmental change and lacustrinegeochemical processes. The overarching objective of the proposed study is to understand hydrochemicalevolution and how it interacts with various environmental controls at different time scales. The addedbonus for undertaking such a study in this climate-sensitive region near the northern limit of the EastAsian monsoon is to improve our ability to read the lacustrine sediment record of this region to betterunderstand the past environmental changes. We propose to use a multidisciplinary approach to investigateat regional and watershed scales, the modern processes in these two lakes, history of solute and water fluxfrom mineralogy and chemical and isotopic composition of authigenic and biogenic minerals, and fromspecies assemblage of ostracodes and the history of climate and environmental change from such recordsof landscape processes as pollen, plant macrofossils, and environmental magnetism.The results from this project will provide insights into understanding the pathways and mechanisms oflake solute evolution and water flux and how they affect the sedimentary record of past environmentalchanges. This is the first study to employ a multidisciplinary approach to address the lake-climateinteractions in Central Asia. A key feature of this project is in its use of paired limnologically- andchemically-contrasting lakes in order to unravel the interactions between lacustrine hydrologic andhydrochemical processes and environmental (and climatic) changes. The study of modern responses ofthe dilute lake (Keluke Lake) with a saline Lake (Toson Lake) will enable comprehensive and robustreconstructions of paleohydrochemistry. Also, the multiple techniques used in the proposed study willprovide independent records of regional climate change, watershed stability and vegetation, as well aschanges in lake chemistry. Integration of these records will allow us to focus on the complex interactionsand feedbacks between these processes at different temporal scales (from present-day to interglacialglacialcycles).Broader impacts. Our interdisciplinary research will advance the understanding of complex interactionsin these systems under different climate regimes. Understanding the lake and watershed responses toclimate change of the past will contribute to our ability to predict the environmental consequences ofclimate (especially monsoon) variations and variability. Our approach of using contrastinghydrochemistries of paired fresh and saline lakes is not commonly employed but we believe is a veryinstructive one with a large pay-off. Understanding the hydrological dynamics will benefit the people inthis remote arid part of China in adapting to the potential future changes in climate and hydrologicalcycles. The results will be compared with the response of lakes in the semi-arid northern Great Plains toclimate and hydrololgic changes and shared with the state geological surveys and water commissions.Once past the pilot-stage, graduate and undergraduate students will be more fully involved in the projectand will benefit from interacting with an international multidisciplinary research team. The project willfacilitate collaborations, especially with our Chinese colleagues, who are having increased impacts in theinternational scene of science and technology.