中国第38次南极科学考察(2021-2022年)南极半岛酸碱度（pH）分水层分析数据

酸碱度描述的是水溶液酸碱性强弱程度，用符号pH来表示。海水pH值是研究二氧化碳体系时易于直接测定的最重要的物理量之一，大洋海水的pH值主要由海水中的碳酸盐体系控制，也受温度、盐度和压力等因素的影响。
中国第38次南极科学考察期间，开展了南极半岛重点海域海水分水层酸碱度(pH)的调查。本数据包括总计22个站(次)的海水酸碱度(pH)分水层数据，水深范围为0-2000m。

pH is a quantitative measure of the acidity and alkalinity of an aqueous solution. Seawater pH is one of the most critical physical parameters that can be directly and conveniently measured during carbon dioxide system research. The pH of open-ocean seawater is primarily governed by the carbonate system dissolved in seawater, and is also influenced by factors including temperature, salinity, and pressure.

During the 38th Chinese National Antarctic Research Expedition, a survey of water-layer seawater pH was conducted in key sea areas around the Antarctic Peninsula. This dataset includes water-layer pH data from a total of 22 stations (casts), with water depths ranging from 0 to 2000 meters.

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背景概述

该数据集包含中国第38次南极科学考察期间在南极半岛22个站点采集的海水酸碱度(pH)分水层数据，覆盖0-2000米水深范围，数据以Excel格式存储，适用于海洋化学研究。