Role of Rainfall on the Geochemical Evolution of Soils: The Atacama Desert of Chile

摘要 土壤形成是一个深刻影响全球大气和水化学的过程，由土壤系统的质量输入和损失的平衡来定义。潮湿地区的观测表明，随着土壤在地质时间尺度上经历生物地球化学变化，风化损失超过了大气输入，并且土壤经历了普遍的生物必需元素化学消耗和大体积塌陷（Vitousek等，1997）。然而，这种模式取决于风化和溶质运输的水的可用性，最近夏威夷的气候比较表明，正如所预期的那样，降水减少导致地质时间跨度内总体质量损失减少（Chadwick 和 Goldstein，2004）。然而，对干旱和超干旱地区土壤的定量质量平衡研究明显缺乏，现阶段很难将这些环境的长期地球化学行为与地球较潮湿的地区进行比较。智力价值。 这项工作与其他研究相结合，将为大气溶质以及随着降水减少而发生的化学和物理风化作用的变化提供一个综合的视角。该提案概述了对智利干旱至超干旱阿塔卡马沙漠降水梯度关键点土壤的年代学研究，与之前公布的数据相结合，将揭示土壤形成如何随着降水减少而经历基本的物理和化学变化。目前，详细的化学和同位素（稳定的宇宙放射性核素）研究已在三个地点启动，研究表明，随着降水量的减少，土壤越来越多地保留大气溶质并经历体积膨胀。然而，这项工作在空间（气候范围）和时间（数百万年前的土壤）上都受到限制。这里需要资金来扩展这项工作，并对土壤学上未勘探的地区形成严格的视角。该项目的主要目标是：（1）沿着智利北部的纬度（降水）梯度开发四个年代序列，（2）量化土壤的化学和物理特性以及沿梯度的大气沉降，以及（3）获得土壤发育的地貌的数值年龄，并在可能的情况下获得土壤本身的数值年龄。这些数据将使我们能够（1）确定土壤随降雨发生的化学和物理变化率，以及（2）为这个独特沙漠中河流特征的地貌演化添加限制。更广泛的影响。 这项工作将通过证明大气沉降对地球土壤的普遍重要性来影响科学，并将提供土壤化学的气候趋势，可以与潮湿地区的其他研究相结合。该项目将影响机构和国际科学交流，因为它将是美国和智利科学家之间的综合合作，将提供学生交流和培训（智利学生到美国，以及美国学生与智利教师和研究生合作），并将提供将由美国和智利同事在智利境内传播的研究成果。最后，该项目的主要资助人员是研究生，这些学生将与不同的合作者密切合作，学生（美国和智利）将接触到的新研究技术将使他们处于地球表面研究技术和概念的前沿。

ABSTRACTSoil formation, a process that profoundly impacts global atmospheric and aqueous chemistry, is defined by the balance of mass inputs to, and losses from, the soil system. Observations in humid regions indicate that as soils undergo biogeochemical alteration over geological time scales, weathering losses exceed atmospheric inputs, and soils experience pervasive chemical depletions of biologically essential elements and large volumetric collapse (Vitousek et al., 1997).Yet this pattern hinges on the availability of water for weathering and solute transport, and recent climate comparisons in Hawaii reveal that decreasing precipitation, as might be expected, results in decreased overall mass losses over geological time spans (Chadwick and Goldstein, 2004).However, there is a decided lack of quantitative mass balance research on the soils of arid andhyperarid regions, and at this stage it is difficult to compare the long-term geochemical behavior of these environments with the Earth.s more humid regions.Intellectual merit. This work, when combined with other research, will provide an integrated perspective of the changing roles of atmospheric solutes and both chemical and physical weathering as precipitation decreases. This proposal outlines a chronological study of soils at critical points along a precipitation gradient in the arid to hyper-arid Atacama Desert of Chile that, when combined with previously published data, will reveal how soil formation undergoes fundamental physical and chemical changes with decreasing precipitation. Presently, detailed chemical and isotopic (stable, cosmogenic radionuclides) studies have been initiated at three locations which reveal that, with decreasing precipitation, soils increasingly retain atmospheric solutes and undergo volumetric expansion. However, this work is restricted in both space (climate range) and time (to multi-million year old soils). Funds are requested here to expand this work and develop a rigorous perspective of a pedologically-unexplored region.The key objectives of this project are to: (1) develop four chronological sequences along a latitudinal (precipitation) gradient in northern Chile, (2) quantify chemical and physical properties of the soils and atmospheric deposition along the gradient, and (3) obtain numerical ages for the landforms on which the soils have developed and, to the extent possible, for the soils themselves.These data will allow us to (1) establish rates of chemical and physical changes in the soils with rainfall and (2) add constraints to the geomorphic evolution of fluvial features in this unique desert.Broader impacts. This work will impact science by demonstrating the pervasive importance of atmospheric deposition to the soils of the Earth, and will provide climatic trends on soil chemistry that can be integrated with other studies in humid areas. The project will impact institutions and international scientific exchange because it will be an integrated collaboration between US andChilean scientists, will provide for student exchange and training (Chilean student to US, and US students working with Chilean faculty and graduate students), and will provide research results that will be disseminated within Chile by both U.S. and Chilean colleagues. Finally, the key funded personnel in the project are graduate students, and these students will work closely with the diverse set of collaborators, and the new research techniques that the students (US and Chilean) will be exposed to will put them at the forefront of earth surface research techniques and concepts.