权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

Collaborative Research: Changes in hyporheic exchange and nitrous oxide generation due to streambed alteration by macro-roughness elements

合作研究：宏观粗糙度元素改变河床引起的流水交换和一氧化二氮生成的变化

基本信息

批准号：
2100927
负责人：
Daniel Tartakovsky
金额：
$ 30万
依托单位：
Stanford University
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2021
资助国家：
美国
起止时间：
2021-08-01 至 2024-07-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=2100927&HistoricalAwards=false
关键词：
Collaborative Research Changes hyporheic exchange

项目摘要

Boulders and large cobbles are ubiquitous roughness elements in mountain rivers and their presence provides vital ecological and hydromorphological functions. They are routinely used in restoration projects to increase habitat quality for many aquatic species because they impact on stream morphology by inducing erosional and depositional areas, whose size and extent depend on the boulder/cobble density, sediment inputs, and flow conditions during sediment mobilizing flows. However, little is known about the role of roughness element induced-streambed changes in regulating hyporheic exchange, which is the process moving stream water into and out of stream bed sediments to form the subterraneous hyporheic zone. The hyporheic zone promotes important biochemical transformations, which affect stream and pore water chemistries with implications at both local and global scales because it is a primary driver of bioactivity in streams and a key source of the greenhouse gas nitrous oxide, N2O. Sustainable management of water resources including river restoration (a $1B/year industry in the US) would benefit from knowledge of hyporheic processes to predict the effects of regulated flows, climate, and land use on ecosystems, nutrient cycles, and solute transport at the local and watershed scales. The scientific goal for this project is to understand, quantify, and model the effects of boulder and cobble density and relative sediment supply during forming flows on hyporheic exchange, chemistry, and N2O production during low flow conditions. This will be addressed with flume and field experiments, supported by analytical and numerical modeling, and tested with hypotheses that boulder or cobble-induced changes in streambed morphology (1) have a primary role in regulating both the quantity and chemistry of hyporheic exchange at the reach scale, and (2) alter aerobic respiration, nitrification, and denitrification rates and increase the rates of apparent production and release of N2O.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.

卵石和大卵石是山区河流中普遍存在的糙率要素，它们的存在提供了重要的生态和水文形态功能。它们通常用于恢复项目，以提高许多水生物种的栖息地质量，因为它们通过诱导侵蚀和沉积区域来影响河流形态，其大小和范围取决于巨石/卵石密度，沉积物输入和沉积物流动过程中的流动条件。然而，很少有人知道的作用，粗糙度元素诱导的河床变化，在调节潜流交换，这是一个过程中移动的河流水进入和流出河床沉积物，形成的subsubwatereous潜流带。潜流区促进重要的生物化学转化，这影响流和孔隙水化学与本地和全球规模的影响，因为它是在流的生物活性的主要驱动力和温室气体一氧化二氮，N2 O的关键来源。水资源的可持续管理，包括河流恢复（美国每年10亿美元的产业）将受益于对潜流过程的了解，以预测受管制流量、气候和土地利用对生态系统、养分循环和局部和流域尺度溶质运移的影响。该项目的科学目标是了解，量化和模拟巨石和卵石密度和相对沉积物供应的影响，在低流量条件下形成流对潜流交换，化学和N2 O生产。这将通过水槽和现场实验来解决，并得到分析和数值模拟的支持，并通过以下假设进行测试：卵石或鹅卵石引起的河床形态变化（1）在调节河段尺度的潜流交换的数量和化学方面具有主要作用，（2）改变有氧呼吸，硝化，和反硝化速率，并增加N2 O的表观生产和释放速率。该奖项反映了NSF的法定使命，并已被认为是值得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的支持。