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营养丰富的海底地下水排放为世界上最大的绿潮提供了燃料。

Nutrient-rich submarine groundwater discharge fuels the largest green tide in the world.

机构信息

Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China; College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao, China.

Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China; Marine Isotope and Geochronology Facility, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.

出版信息

Sci Total Environ. 2021 May 20;770:144845. doi: 10.1016/j.scitotenv.2020.144845. Epub 2021 Jan 21.

Abstract

One of the largest "green tide" (Ulva prolifera) outbreaks in the world has occurred every year from 2007 to present in the Southern Yellow Sea, China. Currently, the coastal area around Jiangsu Province (Subei Shoal region) is thought to be the origination point of these giant green tide blooms. The combination of high nutrient demand but low river discharge and other inputs suggests that there is a significant flux of submarine groundwater discharge (SGD) in this area. By using a radium mass balance model, we estimated the SGD flux in the area to be (0.7-1.4) × 10 m d (6.1-12 cm d), at the high end of SGD fluxes worldwide. Geographically, Subei Shoal is less than 5% of the entire Southern Yellow Sea area, while our calculated SGD flux just for the shoal area is ~3 times larger than previously documented for the whole Southern Yellow Sea. Therefore, Subei Shoal may be considered a SGD hotspot that plays an important role in SGD associated material fluxes. Compared to inputs from local rivers, atmospheric deposition, and anthropogenic activities, SGD-derived nutrients are the main source term that can support the growth of macroalgae. We specifically highlight that this type of areas that are shallow, intensively mixed, anthropogenically polluted, sandy or muddy with heavy bio-irrigation, may have a higher risk of suffering harmful ecological problems, even with limited terrestrial runoff.

摘要

自 2007 年以来,中国黄海每年都会发生世界上最大规模的“绿潮”(浒苔)爆发之一。目前,江苏省沿海地区(苏北浅滩地区)被认为是这些巨型绿潮爆发的起源地。高营养需求但低河流流量和其他输入的组合表明,该地区存在大量的地下水排泄(SGD)。通过使用镭质量平衡模型,我们估计该地区的 SGD 通量为(0.7-1.4)×10 m d(6.1-12 cm d),处于全球 SGD 通量的高端。从地理位置上看,苏北浅滩不到整个黄海面积的 5%,而我们仅为浅滩地区计算的 SGD 通量就比以前记录的整个黄海的通量高出约 3 倍。因此,苏北浅滩可能被视为一个 SGD 热点,在与 SGD 相关的物质通量中起着重要作用。与当地河流、大气沉降和人为活动的输入相比,SGD 来源的营养物质是支持大型藻类生长的主要来源。我们特别强调,这种浅海、强烈混合、人为污染、沙质或泥质、生物灌溉严重的地区,即使陆地径流量有限,也可能面临更高的遭受有害生态问题的风险。

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