Collaborative Research: Towards a Weathering Science Consortium: Two Conferences on Biogeochemistry of the Critical Zone

合作研究：迈向风化科学联盟：关键区生物地球化学的两次会议

• 批准号: 0512398
• 负责人: Donald Sparks
• 金额: --
• 依托单位: University of Delaware
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2005
• 资助国家: 美国
• 起止时间: 2005-04-01 至 2009-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0512398&HistoricalAwards=false
• 关键词: Collaborative; Research; Towards; Weathering; Science

The world's soil resource is probably second only to water in terms of its importance to human society. The rates and mechanisms of processes within the soil zone have a significant impact on events throughout Earth's systems; for example, these processes contribute to nutrient cycling and neutralize acidic precipitation in watersheds. Despite the importance of the soil resource, estimates of soil formation rates are based upon unproven assumptions of steady state and vary widely. However, all estimates agree on a common point: the current estimates of soil erosion rates are one to three orders of magnitude greater than estimates of average soil formation rates, a disturbing conclusion considering the importance of soils to society.The scientific merit of this proposal lies in addressing a clear need for a better system tracking and disseminating information regarding weathering and soil formation. Our proposed initiative will investigate the following question: How does Earth's weathering engine transform rock into soil to nourish ecosystems, shape terrestrial landscapes, and control atmospheric carbon dioxide? The answer requires coupling physical, chemical, and biological processes over a range of spatial and temporal scales and involves a variety of scientific and engineering disciplines.Traditionally, terrestrial low-temperature geochemists and soil chemists have worked in small, single or double PI projects. Very few large, multi-PI projects that cross scales and disciplines have developed from within this community. In contrast, among other scientific communities, large programs have developed to organize scientists into coordinated multi-university teams. For example, IRIS and COSEE have been extremely successful in generating enthusiasm and interest in the seismology and oceanography communities. We propose a new paradigm, a Weathering System Science Consortium (WSSC), to forge this type of multi-PI approach to weathering science and environmental biogeochemistry among terrestrial low-temperature geochemists and soil chemists/biologists. To lay the groundwork for the proposed WSSC, we are requesting funding for two workshops, a symposium at the 18th World Congress of Soil Science in 2006 in Philadelphia that will feature leading scientists who will discuss research frontiers and needs concerning the critical zone, and a database specialist. The current vision for WSSC incorporates four components: 1) a set of "node" sites for data collection; 2) a network of "backbone" soil sites that will be investigated for a standard set of weathering parameters over a range of depths; 3) technical support for instrument and sample node sites and backbone sites and coordinated data management and sample storage systems; and 4) the integration of these efforts through a variety of community-building approaches. The broader impacts of this funding request include the following: 1) improved understanding of the current diversity of questions within the fields of weathering science and environmental biogeochemistry; 2) improved understanding by US scientists of weathering initiatives occurring abroad; 3) development of a coordinated plan to quantify weathering rates in diverse settings; 4) development of a plan to standardize data gathering in the field of weathering science; 5) development of a plan to store and disseminate data from weathering sites worldwide for use by the entire natural sciences community; and 6) organization of the scientific community to investigate fundamental questions in weathering science with great relevance to human society and natural ecosystems.

就其对人类社会的重要性而言，世界土壤资源可能仅次于水。土壤带内的进程速率和机制对整个地球系统的事件有重大影响;例如，这些进程有助于养分循环和中和流域的酸性降水。尽管土壤资源的重要性，土壤形成率的估计是基于未经证实的假设的稳定状态和差异很大。然而，所有的估计都有一个共同点：目前对土壤侵蚀率的估计比平均土壤形成率的估计高出一至三个数量级，考虑到土壤对社会的重要性，这是一个令人不安的结论，这一建议的科学价值在于解决了一个明确的需要，即更好的系统跟踪和传播有关风化和土壤形成的信息。我们提出的倡议将调查以下问题：地球的风化引擎如何将岩石转化为土壤，以滋养生态系统，塑造陆地景观，并控制大气中的二氧化碳？答案需要在一系列空间和时间尺度上耦合物理，化学和生物过程，涉及各种科学和工程学科。传统上，陆地低温地球化学家和土壤化学家在小型，单个或双PI项目中工作。在这个社区中，很少有跨规模和学科的大型多PI项目。相比之下，在其他科学界，大型项目已经发展到将科学家组织成协调的多大学团队。例如，IRIS和COSEE非常成功地激发了地震学和海洋学界的热情和兴趣。我们提出了一个新的范例，一个风化系统科学联盟（WSSC），打造这种类型的多PI方法，在陆地低温地球化学家和土壤化学家/生物学家之间的风化科学和环境地球化学。为了为拟议中的WSSC奠定基础，我们正在申请两个研讨会的资金，一个是2006年在费城举行的第18届世界土壤科学大会上的研讨会，该研讨会将邀请顶尖科学家讨论有关临界区的研究前沿和需求，还有一位数据库专家。目前对WSSC的设想包括四个组成部分：1）一套数据收集的“节点”站点; 2）一个“骨干”土壤站点网络，将对一套不同深度的标准风化参数进行调查; 3）对仪器和样品节点站点和骨干站点以及协调的数据管理和样品存储系统提供技术支持;（4）通过各种社区建设办法将这些努力结合起来。这一资金申请的更广泛影响包括：1）提高对当前风化科学和环境地球化学领域内问题多样性的理解; 2）提高美国科学家对国外风化倡议的理解; 3）制定一项协调计划，以量化不同环境下的风化率;（4）制定风化科学领域数据收集标准化计划;（5）制定存储和传播世界各地风化站点数据的计划，供整个自然科学界使用;组织科学界研究与人类社会和自然生态系统密切相关的风化科学基本问题。