Network Cluster: Patterns and controls of ecohydrology, CO2 fluxes, and nutrient availability in pedogenic carbonate-dominated dryland critical zones
Network Cluster: Patterns and controls of ecohydrology, CO2 fluxes, and nutrient availability in pedogenic carbonate-dominated dryland critical zones
批准号:
2012475
负责人:
Lixin Jin
金额:
$526.93万
依托单位国家:
美国
项目类别:
Cooperative Agreement
财政年份:
2020
资助国家:
美国
项目状态:
未结题
起止时间:
2020-09-01 至 2025-08-31
中文摘要
临界区是地球表面从树木顶部到地下水底部的一层。岩石、土壤、水、空气和生物体在临界区相互作用,提供维持生命的资源,如食物和水。干旱和半干旱气候的旱地占地球面积的45%,为20多亿人提供家园。美国西部的旱地正面临着全球变化造成的重大挑战,如干旱和植物群落的变化。人口和粮食需求的增加也使该地区许多天然旱地变成了灌溉农场。土地使用和气候的这些变化极大地影响了水、碳、养分和盐在旱地不同地区的流动。所有这些变化都影响到自然和农业生态系统的可持续性。这个项目将调查这些重要的关键区域过程,并提高我们预测未来变化的能力。具体而言,这一专题组将调查旱地土壤中的碳酸盐矿物如何控制和影响水、养分、盐和碳进出临界区。该项目将帮助教育和培训初中到高中学生,大学本科生和研究生。这些学生将获得成为科学,技术,工程,艺术和数学(STEAM)未来专业人士的动力,技能和工具。我们的研究和教育工作还将有助于提高公众对旱地临界区功能和服务重要性的认识,旱地生态系统临界区是地球系统中研究不足但至关重要的一部分。它与中质地区相比,植被稀疏,土壤水分有限但动态,地下水位深,土壤有机质低,碱性pH值和盐沉淀物的积累,特别是成壤碳酸盐,可以发展成厚的钙积层并控制土壤结构。然而,这些系统在临界区研究中的代表性不足,目前的概念模型没有充分处理旱地特有的现象,如成土碳酸盐的发展、沙尘暴、间歇性降水以及水文和地球化学过程的高度时空变异。为了填补这些知识空白,该项目的总体目标是通过研究水和养分供应在调节旱地关键区有机碳和无机碳移动方面的作用,提高我们量化和预测旱地碳预算的能力。具体而言,该项目围绕着成壤碳酸盐在决定包气带水动力学、深层地下水位的潜在补给以及典型旱地景观、皮埃蒙特、干盐湖和灌溉农田中的养分循环方面的多方面作用。这些反过来又推动了关键区结构和陆-气碳交换的演变趋势。我们将通过使用一套全面的工具来解决这些问题,包括涡度协方差塔,深临界区钻探,水文地球物理调查,土壤和水文传感器,同位素分析,同步加速器,地球化学代理和基因测序。该项目建立在Jornada LTER,Reynolds Creek CZO,爱达荷州USDA-ARS金伯利站点以及德克萨斯州格兰德河沿着灌溉农业站点的丰富历史数据,知识和模型的基础上。这一专题组将制定一个跨学科框架,以了解旱地关键区的物质和能量流动,并为管理关键区的功能、演变和服务奠定基础,该项目由关键区合作网络和地球科学司水文科学项目联合资助,该奖项反映了NSF的法定使命,并被认为是值得通过使用基金会的智力价值和更广泛的影响审查标准进行评估的支持。
英文摘要
The Critical Zone is the layer of Earth’s surface from the top of the trees to the bottom of the groundwater. Rocks, soil, water, air, and living organisms interact in the Critical Zone to provide life-sustaining resources such as food and water. Drylands, with arid to semi-arid climates, cover 45% of the Earth and provide homes to more than 2 billion people. The drylands of the American West are facing significant challenges caused by global change, such as drought and changing plant communities. Increases in human population and food demand have also converted many natural drylands in this region to irrigated farms. These changes in land use and climate have greatly affected the movement of water, carbon, nutrients and salt through different parts of the drylands. All of these changes impact the sustainability of natural and agricultural ecosystems. This project will investigate these important Critical Zone processes and improve our ability to predict future change. Specifically, this thematic cluster will investigate how carbonate minerals in dryland soils control and impact water, nutrients, salts, and carbon moving in and out of the Critical Zone. This project will help to educate and train middle to high school students, and college undergraduate and graduate students. These students will be provided with the motivation, skills and tools to become future professionals in science, technology, engineering, arts, and mathematics (STEAM). Our research and education efforts will also help to grow public awareness of the importance of the Critical Zone function and service in drylands.The Critical Zone in dryland ecosystems is an understudied but crucial part of the Earth system. It contrasts with mesic areas by having sparse vegetation, limited but dynamic soil moisture, deep water table, low soil organic matter, alkaline pH, and buildup of salt precipitates, especially as pedogenic carbonates that can develop into a thick caliche layer and dominate the soil structure. However, these systems are underrepresented in Critical Zone research and current conceptual models do not fully address phenomena unique to drylands such as development of pedogenic carbonate, dust storms, episodic precipitation, and high spatiotemporal variability in hydrological and biogeochemical processes. To fill these knowledge gaps, the overarching goal of the project is to increase our capacity to quantify and predict dryland carbon budgets across land-use and climatic gradients by examining the role of water and nutrient availability in regulating the movement of organic and inorganic carbon in the dryland Critical Zone. Specifically, this project centers around the multifaceted roles of pedogenic carbonates in dictating vadose zone water dynamics, the potential recharge to deep water table, and nutrient cycling in typical dryland landscapes, piedmont, playa and irrigated agricultural fields. These in turn drive trends in evolution of Critical Zone architectures and land-atmosphere C exchange. We will tackle these problems by using a comprehensive set of tools including eddy covariance towers, deep Critical Zone drilling, hydrogeophysical surveys, soil and hydrologic sensors, isotopic analysis, synchrotron, geochemical proxies, and genetic sequencing. This project builds on the rich historical data, knowledge, and models at the Jornada LTER, the Reynolds Creek CZO, USDA-ARS Kimberly site in Idaho and irrigated agricultural sites along the Rio Grande Valley in Texas. This thematic cluster will develop an interdisciplinary framework to understand material and energy flow through dryland Critical Zones and lay the foundation for managing Critical Zone function, evolution, and services, as well as forecasting carbon budget changes with future shifts in climate and land use in drylands.This project is jointly funded by the Critical Zone Collaborative Network and the Hydrologic Sciences programs in the Division of Earth Sciences and the Hispanic Serving Institutions program in the Education and Human Resources Directorate's Division of Human Resource Development.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.
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财政年份:2024
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批准号:1853680
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财政年份:2016
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