海洋酸化:另一个行星边界被越过
Helen S Findlay1, Richard A Feely2, Li-Qing Jiang3,4
1Plymouth Marine Laboratory, Plymouth, UK.
Global change biology
|June 9, 2025
概括
海洋酸化正在接近一个关键的行星边界,影响海洋生物. 全球海洋已经超过了这个界限,威胁到生态系统和化物种息地.
科学领域:
- 环境科学 环境科学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 海洋酸化是行星边界框架中确定的一个关键的行星过程.
- 目前的条件接近于可能引发不可接受的环境变化的边界.
研究的目的:
- 用更新的数据和模型重新评估海洋酸化的行星边界.
- 评估海洋酸化对海洋生态系统和息地的影响.
主要方法:
- 使用了经过修订的工业化前阿拉戈尼特和状态估计.
- 采用最先进的数据模型产品,包含不确定性.
- 对生态指标和化物种息地的评估影响.
主要成果:
- 到2020年,全球平均海洋状况将超过海洋酸化极限.
- 全球地下海洋 (至200米) 的高达60%和表面海洋的40%以上越过了边界.
- 对珊瑚 (43%),类动物 (61%) 和双动物 (13%) 观察到显著的息地减少.
结论:
- 为了防止生态系统风险,建议从工业化前条件减少10%的修订边界.
- 到2000年,表面海洋已经超过了这一修订的基准值.
- 迫切需要采取行动,减轻海洋酸化,保护海洋生态系统和服务.
相关概念视频
Acid–Base Equilibria: Activity-Based Definition of pH
561
For an ideal solution, the pH is defined as the negative logarithm of the hydrogen ion concentration. For a non-ideal solution, an accurate measurement of the pH must consider the negative logarithm of the hydrogen ion activity rather than concentration. In such a solution, the pH can be more accurately defined as the negative logarithm of a product of the hydrogen ion concentration and its activity coefficient.
In solutions of very low ionic strength—for example, pure water—the...
In solutions of very low ionic strength—for example, pure water—the...
561
Disorders of Acid-Base Balance
161
The human body maintains a precise pH range of arterial blood between 7.35 and 7.45. Deviations result in either acidosis (pH < 7.35) or alkalosis (pH > 7.45). These conditions are further classified as respiratory or metabolic disorders based on their underlying cause.
Respiratory Acidosis and Alkalosis
Respiratory acidosis occurs due to an increase in the partial pressure of carbon dioxide PCO2 in the blood. It often arises from shallow breathing or impaired gas exchange caused by...
Respiratory Acidosis and Alkalosis
Respiratory acidosis occurs due to an increase in the partial pressure of carbon dioxide PCO2 in the blood. It often arises from shallow breathing or impaired gas exchange caused by...
161
The Carbon Cycle
37.1K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
37.1K
pH Scale
68.5K
Hydronium and hydroxide ions are present both in pure water and in all aqueous solutions, and their concentrations are inversely proportional as determined by the ion product of water (Kw). The concentrations of these ions in a solution are often critical determinants of the solution’s properties and the chemical behaviors of its other solutes. Two different solutions can differ in their hydronium or hydroxide ion concentrations by a million, billion, or even trillion times. A common means of...
68.5K
The Phosphorus Cycle
36.6K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
36.6K
pH
133.3K
The potential of hydrogen (pH) is a measure of the acidity or basicity of a water-based solution determined by the concentration of hydronium ions (H3O+). In one liter of pure water at neutral pH, there are 1×10−7 moles of hydronium ions. However, the extensive range of hydronium ion concentrations present in water-based solutions makes measuring pH in moles cumbersome. Therefore, a pH scale was developed to convert moles of hydronium ions into the negative logarithm of the hydronium...
133.3K


