Investigation of Dominant Controls on Electrical Properties of Granitic Regolith

地球的关键地带是从基岩顶部延伸到树冠的薄层。尽管它的厚度相对较薄，但它在我们的社会中发挥着至关重要的作用，它提供了维持生命的资源，如水和食物。了解临界带地下部分的内部结构是帮助我们理解和预测其在全球水、能源、碳和营养循环中的作用的重要一步。地球物理成像是用来“看到”地表下看不见的临界区。然而，获得的地球物理图像需要转化为其他科学家可以理解和使用的物理特性，如密度、水分含量和化学成分。该项目将通过实验室和地球物理实地调查相结合，推进目前对关键地带地质物质物理性质的理解。这个项目的结果将帮助科学家更好地描绘这个薄而宝贵的地球关键带层的地下。研究人员将通过现场采样、实验室实验和理论建模相结合的方法来研究花岗岩风化层电学性质的主要控制因素。将从野外采集花岗质风化层样品，并使用新开发的土柱和配备新型水文地球物理探测器的压力板提取器测量其在受控水力状态下的电学特性。实验数据将用于量化水力状态、化学风化引起的结构变化和化学风化引起的矿物学变化对完全发育的风化层和风化前沿样品电学性能的相对影响。将建立一个综合化学风化作用的新电模型来描述整个风化层。这种基于过程的理解和建模将增强我们观察复杂地下环境和监测各种重要地下过程的能力。该项目由水文科学、刺激竞争性研究的既定计划（EPSCoR）以及地球生物学和低温地球化学计划共同资助。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。

The Earth's critical zone is the thin layer that extends from the top of the bedrock to the canopy of trees. Despite its relatively thin thickness, the critical zone plays a vital role in our society by providing life-sustaining resources such as water and food. Knowing the internal structure of the underground part of the critical zone is an important step that will help us understand and predict its role in global water, energy, carbon, and nutrient cycles. Geophysical imaging is used to "see" the unseen critical zone underneath the surface. However, the acquired geophysical images need to be translated into physical properties such as density, moisture content, and chemical composition that are understandable and usable to other scientists. This project will advance current understanding of the physical properties of geological materials in the critical zones by using a combination of laboratory and geophysical field investigations. The outcome of this project will help scientists better depict the subsurface of this thin but invaluable critical zone layer of the Earth. The researchers will investigate the dominant controls on the electrical properties of granitic regolith from a combination of field sampling, laboratory experiments, and theoretical modeling. Granitic regolith samples will be collected from the field, and their electrical properties, under controlled hydraulic states, will be measured using a newly developed soil column and a pressure plate extractor equipped with novel hydro-geophysical probes. Experimental data will be used to quantify the relative influences of hydraulic state, chemical weathering-induced textural change, and chemical weathering-induced mineralogy alternation on the electrical properties of the samples in both fully developed regolith and the weathering front. A new electrical model integrating chemical weathering will be developed to describe the entire regolith. This process-based understanding and modeling will enhance our ability to see into the complex underground environment and monitor various important subsurface processes. This project is jointly funded by the Hydrologic Sciences, the Established Program to Stimulate Competitive Research (EPSCoR), and Geobiology and Low Temperature geochemistry programs.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.