Zhu Tianqiang, Zheng Liwen, Li Feng, Liu Jihua, Zhuang Wen
Institute of Marine Science and Technology, Shandong University, Qingdao 266237, China; School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China; National Laboratory for Marine Science and Technology, Qingdao 266237, China; Institute of Eco-environmental Forensics, Shandong University, Qingdao 266237, China.
Institute of Marine Science and Technology, Shandong University, Qingdao 266237, China.
Sci Total Environ. 2024 Jun 20;930:172853. doi: 10.1016/j.scitotenv.2024.172853. Epub 2024 Apr 27.
Enhancing silicate weathering to increase oceanic alkalinity, thereby facilitating the absorption of atmospheric carbon dioxide (CO), is considered a highly promising technique for carbon sequestration. This study aims to evaluate the feasibility and potential of olivine-based ocean alkalinity enhancement (OAE) for the removal of atmospheric CO and its storage in seawater as bicarbonates in the East and South China Seas (ESCS). A particular focus is placed on the potential ecological impacts arising from the release of nickel (Ni) and chromium (Cr) during the olivine weathering process. We considered two extreme scenarios: one where Ni and Cr are entirely retained in seawater, and another where they are completely deposited in sediments. These scenarios respectively represent the maximum permissible concentrations of Ni and Cr in seawater and sediments during the OAE process. Current marine environmental quality standards (EQS) were utilized as the threshold limits for Ni and Cr in both seawater and sediment, with concentrations exceeding these EQS potentially leading to significant adverse effects on marine life. When all released Ni is retained in seawater, the allowable dosage of olivine varies from 0.05 to 13.7 kg/m (depending on olivine particle size, temperature, and water depth); when all released Ni is captured by sediment, the permissible addition of olivine ranges from 0.21 to 2.1 kg/m (depending on mixing depth). Given the low solubility of Cr, it is not necessary to consider the scenario where Cr exceeds the limit in seawater. The allowable amount of Cr entirely retained in sediments ranges from 0.69 to 47.2 kg/m.In most scenarios, the accumulation of metals in sediments preferentially exceeds the corresponding threshold value rather than remaining in seawater. Therefore, we recommend using alkalization equipment to fully dissolve olivine before discharging into the sea, enabling a larger-scale application of olivine without significant negative ecological impacts.
增强硅酸盐风化以提高海洋碱度,从而促进大气中二氧化碳(CO)的吸收,被认为是一种极有前景的碳封存技术。本研究旨在评估基于橄榄石的海洋碱度增强(OAE)技术在东中国海和南中国海(ESCS)去除大气中CO并将其以碳酸氢盐形式存储于海水中的可行性和潜力。特别关注橄榄石风化过程中镍(Ni)和铬(Cr)释放所产生的潜在生态影响。我们考虑了两种极端情况:一种是Ni和Cr完全保留在海水中,另一种是它们完全沉积在沉积物中。这些情况分别代表了OAE过程中海水和沉积物中Ni和Cr的最大允许浓度。当前的海洋环境质量标准(EQS)被用作海水和沉积物中Ni和Cr的阈值限制,超过这些EQS的浓度可能会对海洋生物产生重大不利影响。当所有释放的Ni都保留在海水中时,橄榄石的允许用量从0.05到13.7千克/立方米不等(取决于橄榄石粒径、温度和水深);当所有释放的Ni都被沉积物捕获时,橄榄石的允许添加量范围为0.21到2.1千克/立方米(取决于混合深度)。鉴于Cr的溶解度较低,无需考虑Cr在海水中超过限值的情况。完全保留在沉积物中的Cr的允许量范围为0.69到47.2千克/立方米。在大多数情况下,沉积物中金属的积累优先超过相应的阈值,而不是留在海水中。因此,我们建议在将橄榄石排放到海中之前,使用碱化设备将其充分溶解,以便在不产生重大负面生态影响的情况下更大规模地应用橄榄石。