The rate of respiration in aquatic organisms is
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Respiration is the process by which organisms obtain oxygen and release carbon dioxide. The rate of respiration depends on the availability of oxygen in the environment.
Oxygen is much less available in water than in air. Water contains dissolved oxygen, but its concentration is low. For example, at 20°C, water holds about 9 mg/L of oxygen, while air contains about 210 mg/L of oxygen. This is represented by the formula for dissolved oxygen concentration, which is dependent on temperature and pressure.
Formula for dissolved oxygen saturation: , where is the saturation concentration, is a constant dependent on temperature, and is the partial pressure of oxygen.
Due to lower oxygen availability, aquatic organisms often have slower metabolic rates and respiration rates compared to terrestrial and aerial organisms. They may need to expend more energy to extract oxygen from water (e.g., through gills with high surface area and constant water flow).
Given the lower oxygen concentration in water, the rate of respiration in aquatic organisms is generally slower than in terrestrial and aerial organisms, where oxygen is more abundant and easier to obtain.
The correct statements are:
Diffusion and Gas Exchange: Oxygen moves into organisms via diffusion. The rate of diffusion is faster in air than in water due to higher concentration gradients and lower resistance.
Adaptations: Aquatic organisms have adaptations like gills and counter-current exchange systems to maximize oxygen uptake, but their respiration rates are still limited by the environment.
Fick's Law of Diffusion: , where is the diffusion flux, is the diffusion coefficient (lower in water), is the area, and is the concentration gradient.