Collaborative Research: How do interactions of transport and stoichiometry maximize stream nutrient retention?

合作研究:运输和化学计量的相互作用如何最大限度地保留河流养分?

基本信息

  • 批准号:
    1642403
  • 负责人:
  • 金额:
    $ 12.02万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2017
  • 资助国家:
    美国
  • 起止时间:
    2017-07-15 至 2021-06-30
  • 项目状态:
    已结题

项目摘要

There is considerable exchange of water and solutes among four compartments of streams: the fast moving part of the stream channel, in-channel storage zones, and shallow and deep sediments zones. Exchanges of water between these compartments promote dissolved nutrient reactions and removal. The team hypothesizes that nutrient reaction in streams is controlled by not only hydrologic transport, but also stoichiometry of nutrients (ratio of C:N:P). The team will test their hypotheses by conducting field data collection and stream solute injections at three contrasting Critical Zone Observatory (CZO) sites (Boulder Creek, a rocky mountain setting in Colorado; Catalina-Jemez, a low nutrient setting in New Mexico; and an agricultural landscape in Iowa). Across these three sites there is substantial variability in geology, hydrology, and background nutrient concentrations (and therefore nutrient limitations). The project will engage multiple graduate students with an emphasis on diversity. The team will also organize a workshop to promote and stimulate interaction and exchange of ideas and knowledge among the principal players in the stream restoration field, particularly young scientists and practitioners, stream restoration companies and local environmental agencies.The exchange of water and solutes among the river and its hyporheic zones result in a net reaction and removal on nutrients from the stream. Nutrient reaction and removal (carbon, nitrogen, and phosphorous) in streams is limited by not only the biomass available to take up nutrients, but is also stoichiometrically limited by the specific reaction. This project will work with the hypothesis that: (1) nutrient retention in streams is controlled by not only hydrologic transport, but also stoichiometry of nutrients (ratio of C:N:P); (2) each compartment of a stream (main channel, surface storage, shallow/deep hyporheic) has a different optimal stoichiometric need (i.e., C:N:P); and (3) depletion of dissolved oxygen from aerobic metabolism is a first-order control that causes a threshold change in the stoichiometric demand of C, N, and P as a compartment becomes anoxic and biogeochemical processes change. The concepts will be tested by conducting field data collection and stream solute injections at three contrasting Critical Zone Observatory (CZO) sites across variable hydrologic conditions at each site to test over a range of hydrologic transport conditions. The team will deploy a suite of methods including electrical resistivity imaging, nutrient tracer injections based on stoichiometric tradeoffs, the Tracer Additions for Spiraling Curve Characterization (TASCC method), application of the "smart" tracer resazurin in streams and use of shallow (MINIPOINT samplers) and deep (wells) hyporheic flow paths. Nutrient tracer injections are designed to specifically decipher stoichiometric controls on nutrient retention in each of the four compartments of the streams. The broader impacts will be communicated in a workshop setting that identifies reciprocal needs from academic research and restoration programs seeking to approach stream restoration projects more holistically.
在河流的四个区间,水和溶质有相当大的交换:河道的快速流动部分,河道内储存区,浅层和深层沉积物区。这些隔室之间的水交换促进溶解的营养反应和去除。研究小组假设,河流中的营养反应不仅受到水文运输的控制,还受到营养物质化学计量学(C:N:P的比例)的控制。研究小组将通过在三个不同的关键区域观测站(CZO)进行实地数据收集和溪流溶质注入来验证他们的假设(Boulder Creek,科罗拉多州的岩石山环境;Catalina-Jemez,新墨西哥州的低营养环境;以及爱荷华州的农业景观)。在这三个地点,在地质、水文和背景营养浓度(因此营养限制)方面存在很大的差异。该项目将吸引多名研究生参与,重点是多样性。该小组亦会举办工作坊,促进和鼓励溪流修复界的主要人士,特别是青年科学家和实践者、溪流修复公司和本地环保机构之间的互动和交流思想和知识。河流及其潜流带之间的水和溶质交换导致净反应和从河流中去除营养物质。营养物的反应和去除(碳、氮和磷)不仅受到可吸收营养物的生物量的限制,而且在化学计量上也受到特定反应的限制。该项目将基于以下假设:(1)河流中的营养物质保留不仅受水文运输控制,而且受营养物质化学计量学(C:N:P比)控制;(2)河流的每个隔室(主河道、地表水库、浅/深潜流)具有不同的最佳化学计量需求(即C:N:P);(3)有氧代谢中溶解氧的消耗是一阶控制,当隔室缺氧和生物地球化学过程发生变化时,会导致C、N和P的化学计量需求发生阈值变化。这些概念将通过在三个不同水文条件的关键区域观测站(CZO)进行现场数据收集和溪流溶质注入来进行测试,以测试每个站点在一系列水文运输条件下的变化。该团队将部署一套方法,包括电阻率成像、基于化学计量学权衡的营养示踪剂注射、用于螺旋曲线表征的示踪剂添加(TASCC方法)、在溪流中应用“智能”示踪剂resazurin,以及使用浅(MINIPOINT采样器)和深(井)的潜流路径。营养示踪剂注射剂的设计是专门破译化学计量控制的营养保留在每四个隔间的溪流。更广泛的影响将在研讨会上进行交流,以确定学术研究和修复项目的相互需求,寻求更全面地处理河流修复项目。

项目成果

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Kamini Singha其他文献

Correction: Geostatistical Rock Physics Inversion for Predicting the Spatial Distribution of Porosity and Saturation in the Critical Zone
  • DOI:
    10.1007/s11004-022-10010-4
  • 发表时间:
    2022-07-11
  • 期刊:
  • 影响因子:
    3.600
  • 作者:
    Dario Grana;Andrew D. Parsekian;Brady A. Flinchum;Russell P. Callahan;Natalie Y. Smeltz;Ang Li;Jorden L. Hayes;Brad J. Carr;Kamini Singha;Clifford S. Riebe;W. Steven Holbrook
  • 通讯作者:
    W. Steven Holbrook
Real-time monitoring of emin situ/em chemical oxidation (ISCO) of dissolved TCE by integrating electrical resistivity tomography and reactive transport modeling
通过整合电阻率层析成像和反应性输运模型对溶解态三氯乙烯的原位化学氧化(ISCO)进行实时监测
  • DOI:
    10.1016/j.watres.2024.121195
  • 发表时间:
    2024-03-15
  • 期刊:
  • 影响因子:
    12.400
  • 作者:
    Zheng Han;Xueyuan Kang;Kamini Singha;Jichun Wu;Xiaoqing Shi
  • 通讯作者:
    Xiaoqing Shi

Kamini Singha的其他文献

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{{ truncateString('Kamini Singha', 18)}}的其他基金

Collaborative Research: How roots, regolith, rock and climate interact over decades to centuries — the R3-C Frontier
合作研究:根系、风化层、岩石和气候在数十年至数百年中如何相互作用 - R3-C 前沿
  • 批准号:
    2121659
  • 财政年份:
    2021
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
Collaborative Research: Network Cluster: Bedrock controls on the deep critical zone, landscapes, and ecosystems
合作研究:网络集群:对深层关键区域、景观和生态系统的基岩控制
  • 批准号:
    2012408
  • 财政年份:
    2020
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
CZ RCN: Expanding knowledge of the Earth's Critical Zone: connecting data to models
CZ RCN:扩展地球关键区域的知识:将数据连接到模型
  • 批准号:
    1904527
  • 财政年份:
    2019
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Standard Grant
Collaborative Research: Emergent Hydrological Properties Associated with Multiple Channel-Spanning Logjams
合作研究:与多航道堵塞相关的新兴水文特性
  • 批准号:
    1819134
  • 财政年份:
    2018
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
Laboratory Technician Support: Expanding Capabilities for Experimental Hydrogeophysics Research and Outreach
实验室技术人员支持:扩大实验水文地球物理研究和推广的能力
  • 批准号:
    1824330
  • 财政年份:
    2018
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
Collaborative Research: Calibrating Shallow Geophysical Techniques to Detect Large Wood Buried in River Corridors
合作研究:校准浅层地球物理技术以检测埋在河流走廊中的大型木材
  • 批准号:
    1612983
  • 财政年份:
    2016
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Standard Grant
Collaborative Research: Revealing the Role of Less-Mobile Porosity in Hyporheic Denitrification and Greenhouse Gas Production
合作研究:揭示流动性较差的孔隙在潜流反硝化和温室气体产生中的作用
  • 批准号:
    1446375
  • 财政年份:
    2015
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
Collaborative Research: From Roots to Rock - Linking Evapotranspiration and Groundwater Fluxes in the Critical Zone
合作研究:从根部到岩石 - 将关键区域的蒸散量和地下水通量联系起来
  • 批准号:
    1446231
  • 财政年份:
    2015
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Continuing Grant
Collaborative Research: Unraveling Transport in Porous Media through the Integration of Isotopic Tracers, Geophysical Data, and Numerical Modeling
合作研究:通过同位素示踪剂、地球物理数据和数值模拟的集成来揭示多孔介质中的输运
  • 批准号:
    1446235
  • 财政年份:
    2015
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Standard Grant
Early Career: Acquisition of Instrumentation to Measure Electrical Resistivity at the Field and Lab Scale
早期职业生涯:购买仪器以在现场和实验室规模测量电阻率
  • 批准号:
    1338461
  • 财政年份:
    2013
  • 资助金额:
    $ 12.02万
  • 项目类别:
    Standard Grant

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