Collaborative Research: Sediment Geochemical Control on Ocean Acidification and Carbon Budget in a River Dominated Shelf System

在许多沿海地区，化肥被冲下河流，导致藻类大量繁殖。在较深的沃茨或沉积物中，藻类产生的有机物质的消耗了氧气，导致墨西哥湾北方等许多地方的低氧“死区”。这种营养物质输入、藻类生长和氧气流失的过程称为富营养化。有机物的消耗也会将溶解的二氧化碳释放到水中，直接或间接地导致海洋酸化。为了了解和预测这种对酸化的影响，重要的是要了解有多少有机物降解发生在水柱中，而不是沉积物中，它在季节和年份之间的变化如何，以及它如何受到风暴等过程的影响。在这个项目中，来自三个机构的研究人员沿着他们的研究生和本科生将进行实地观察和计算机建模相结合，以解决这些问题在墨西哥湾北方。他们将通过当地的外展活动与公众分享他们的成果，并通过与当地教师的合作伙伴关系和课程开发与路易斯安那州的中学生分享他们的成果。拟议的研究将使用一种结合观测和数值模拟的方法，以更好地了解陆架沉积物在驱动底层水溶解无机碳（DIC）和pH动态和季节尺度酸化中的作用。过去和现在的研究都没有涉及这一机制。由于目前缺乏知识，很难为该地区建立一个全面的碳预算。拟议的研究将（一）量化的作用，底栖通量DIC生产导致酸化的底层水;（二）确定的重要性，季节性变化的底栖DIC通量酸化的底层水;和（三）探讨的重要性，情节再悬浮事件在调制底栖DIC通量。将利用最先进的底栖登陆平台在路易斯安那大陆架进行季节性取样，以记录现场沉积物和底层水耗氧率、有机物矿化率、沉积物氧渗透深度、DIC的底栖通量和伴随的pH值下降。还将结合沉积物孔隙水和水柱取样记录底流速度和浊度。为了补充这些详细的近床和海底观测，我们将利用最近开发的耦合流体动力学，沉积物输运和海洋地球化学模型（HydroBioSed），将观测到的底栖通量估计值扩大到年度规模。该奖项反映了NSF的法定使命，并被认为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来支持。

In many coastal regions fertilizer washed down rivers leads to high production of algae. Consumption of organic material produced by the algae in deeper waters or in sediments consumes oxygen, leading to low-oxygen "dead zones" in many places like the northern Gulf of Mexico. This process of nutrient input, algal growth, and loss of oxygen is called eutrophication. Consumption of the organic matter also releases dissolved carbon dioxide into the water, and contributes directly and indirectly to ocean acidification. In order to understand and predict this impact on acidification, it is important to understand how much of the organic matter degradation occurs in the water column versus in the sediments, how variable it is between seasons and years, and how it is affected by processes such as storms that disturb the bottom sediments. In this project, investigators from three institutions along with their graduate and undergraduate students will conduct a combination of field observations and computer modeling to address these questions in the northern Gulf of Mexico. They will share their results with the public through local outreach activities, and with secondary school students in Louisiana through partnerships and curriculum development with local teachers.The proposed research will use a combined observational and numerical modeling approach to better understand the role of shelf sediment in driving bottom water dissolved inorganic carbon (DIC) and pH dynamics and acidification at seasonal scales. Past and current studies have not addressed this mechanism. This current lack of knowledge makes it difficult to construct a comprehensive carbon budget for this region. The proposed research will (i) quantify the role of benthic fluxes in DIC production leading to acidification in the bottom water; (ii) determine the importance of the seasonally changing benthic DIC flux in acidifying the bottom water; and (iii) explore the importance of episodic resuspension events in modulating benthic fluxes of DIC. Seasonal sampling will be carried out in Louisiana shelf using state of the art benthic lander platform to record in situ sediment and bottom water oxygen consumption rates, organic matter remineralization rates, sediment oxygen penetration depths, benthic fluxes of DIC and accompanying pH drop. Bottom current velocities and turbidity will also be recorded in conjunction with sediment porewater and water column sampling. Complementing these detailed near-bed and seabed observations, we will utilize a recently developed coupled hydrodynamics, sediment transport and biogeochemistry model (HydroBioSed) to scale up observed estimates of benthic fluxes to an annual scale.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.