Natural waterbodies are full of plant and algal life, sometimes you can see it and sometimes you can't but it is always there. During the day, the plant and algal life photosynthesize in response to the availability of light. In the process they consume CO2 and release O2, just like terrestrial plants do. The release of O2 into the water column increases the DO concentration (of course) and the consumption of CO2 reduces the potential for the formation of carbonic acid, thus resulting in a more alkaline (higher) pH.
During the night, when there is no UV light available to support photosynthesis, the plants and algae still have to respire (they are alive) which results in the consumption of O2 and release of CO2 into the water column, having the opposite effect to photosynthesis and resulting in the cycling of pH and DO on a day-night (diurnal) basis.
The amount of dissolved oxygen decreases when water temperature increases. Warm water is unable to dissolve as much oxygen gas.
Temperature has a direct effect on the concentration of dissolved oxygen in water. As the temperature of the water increases, the solubility of oxygen decreases and the concentration of dissolved oxygen will decrease. Conversely, as the temperature of the water decreases, the solubility of oxygen increases and the concentration of dissolved oxygen will increase. Additionally, warmer water is generally less dense than colder water, resulting in less efficient oxygen transfer.
Dissolved oxygen is the current amount of oxygen in the water. A certain amount of Dissolved Oxygen Is needed to keep the fish alive, if any of the dissolved oxygen decreases by either a little or a lot it can cause changes in the water, normally if the dissolved oxygen decreases so do the fish and aquatics life's life.
Dissolved oxygen is the current amount of oxygen in the water. A certain amount of Dissolved Oxygen Is needed to keep the fish alive, if any of the dissolved oxygen decreases by either a little or a lot it can cause changes in the water, normally if the dissolved oxygen decreases so do the fish and aquatics life's life.
As the altitude increases, the density of oxygen decreases.
. Temperature directly affects the solubility of oxygen in water. When the temperature of water increases, a portion of oxygen converts from liquid state to a gas. Thus the ability of water to maintain oxygen in dissolved state decreases with increasing temperature. As a result, colder water can potentially contain more dissolved oxygen than warm water. Therefore, a lake in spring contains greater amount of Dissolved Oxygen than the same lake in summer.
only anaerobic(oxygen free) bacteria survives .
there is less oxygen and the molecules are more spread out
Oxygen solubility in water is strange and does not follow "normal" solubility rules along with many other gases. The solubility increases as temperature decreases.
It should be zero. We can use as DO standard solution instead of 2.0 M sodium sulphite (because 2.0 M Na2SO3 DO is zero). Refer to the following link below.
dissolved oxygen is dissolved oxygen
The oxygen dissolved in water is a measure of dissolved oxygen (DO).