Baseline pore-water nutrients, cations and DIC for sediment core SO268/1_74-1 (MUC-17) during RV SONNE cruise SO268/1 in the CCZ, Pacific Ocean@en
收藏资源简介:
This baseline dataset comprises downcore measurements of pore-water nutrients, cations and DIC for a sediment core (MUC) retrieved in the framework of the European collaborative JPI Oceans MiningImpact project onboard R/V SONNE cruise SO268 in 2019. The scientific work during cruise SO268 was part of the second phase of the MiningImpact project (Environmental impacts and risks of deep-sea mining) and is designed to assess the environmental impacts of deep-sea mining of polymetallic nodules in the Clarion-Clipperton Zone (CCZ) in the Pacific Ocean. The pore water was extracted onboard by rhizon sampling. Pore-water nutrient concentrations (nitrate, nitrite, ammonium, silicic acid, phosphate) were analyzed onboard on freshly extracted pore water upon 3-fold dilution or undiluted (ammonium) using a QuAAtro continuous segmented flow analyzer (Seal Analytical). Major and minor elements were determined on acidified samples (25 µL double sub-boiling distilled concentrated HCl per 1 mL sample) using ICP-AES (iCAP 7400, Thermo Scientific) and DIC was determined on HgCl2-treated pore-water samples using a QuAAtro continuous segmented flow analyzer (Seal Analytical) at the Marine Geochemistry Lab, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven.
本基准数据集包含2019年在欧洲联合JPI Oceans框架下的MiningImpact合作项目中,于SONNE号(R/V SONNE)科考船SO268航次采集的沉积物岩芯(MUC)的沿岩芯深度孔隙水营养盐、阳离子及溶解无机碳(Dissolved Inorganic Carbon,DIC)测量数据。SO268航次的科考工作属于MiningImpact项目第二阶段——深海采矿的环境影响与风险的研究内容,旨在评估太平洋克拉里昂-克利珀顿区(Clarion-Clipperton Zone,CCZ)多金属结核深海采矿的环境影响。孔隙水采用根际采样器(rhizon sampling)在科考船上现场提取。孔隙水营养盐(硝酸盐、亚硝酸盐、铵盐、硅酸、磷酸盐)浓度在科考船上对新鲜提取的孔隙水进行分析:其中铵盐采用未稀释样品直接检测,其余营养盐均经3倍稀释后,使用QuAAtro连续流动分析仪(Seal Analytical公司)完成测定。常量及微量元素通过对酸化样品(每1mL样品加入25 μL二次亚沸蒸馏浓盐酸)采用电感耦合等离子体原子发射光谱(Inductively Coupled Plasma Atomic Emission Spectroscopy,ICP-AES,iCAP 7400,Thermo Scientific)完成检测;溶解无机碳(DIC)则采用经氯化汞(HgCl₂)预处理的孔隙水样品,由不来梅港亥姆霍兹极地与海洋研究中心阿尔弗雷德·魏格纳研究所(Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research)海洋地球化学实验室的QuAAtro连续流动分析仪(Seal Analytical公司)完成测定。



