Out of total liquid water on earth, the brackish water is
estimates are not available.
Earth is often called the "Blue Planet" because of the abundance of water on its surface. However, most of this water is saltwater, found in oceans and seas. Only a small fraction is freshwater, which is essential for most human and ecological needs.
To understand where brackish water fits in, let's first look at the overall distribution of Earth's water:
This means that the vast majority of the total liquid water on Earth is saltwater in the oceans.
Even the small percentage of freshwater is not all easily accessible. Freshwater is primarily stored in:
Brackish water is water that has a salinity content between that of freshwater and saltwater. It is saltier than freshwater but not as salty as seawater. The salinity can vary widely depending on the location and conditions.
Brackish water typically occurs where freshwater mixes with saltwater. Common locations include:
Unlike the vast, relatively stable bodies of saltwater (oceans) or the large reservoirs of frozen freshwater (ice caps) and groundwater, brackish water exists in more dynamic, transitional zones. The volume and salinity of brackish water bodies can fluctuate significantly due to factors like:
Because brackish water is found in such diverse and variable environments that represent transition zones rather than distinct, easily quantifiable global reservoirs, obtaining a precise, globally accepted estimate for the total volume of brackish water is challenging. Furthermore, presenting this variable amount as a fixed percentage of the *total liquid water* on Earth (which is overwhelmingly ocean saltwater) is not standard practice in global water distribution models.
While local or regional estimates for specific brackish water bodies might exist, a reliable figure for the total volume of brackish water on Earth as a percentage of the total liquid water is complex to determine and often not precisely quantified or standardized in global hydrological data summaries. Therefore, widely accepted global estimates for the percentage of total liquid water that is brackish water are generally considered unavailable or not precisely defined in standard water resource statistics.
| Water Type | Salinity Level | Common Locations |
|---|---|---|
| Freshwater | Low (typically < 1 ppt) | Rivers, lakes, glaciers, most groundwater |
| Brackish Water | Intermediate (typically 1 to 10 ppt, though definitions vary) | Estuaries, coastal wetlands, some inland seas |
| Saltwater | High (typically > 10 ppt, seawater is ~35 ppt) | Oceans, seas |
| Water Category | Approximate Percentage of Total Water | Approximate Percentage of Total Liquid Water |
|---|---|---|
| Saltwater (Oceans) | 97.5% | > 97% |
| Freshwater (Ice, Groundwater, Surface, etc.) | 2.5% | < 3% |
| Brackish Water | Estimates not widely available as a global percentage of total water or total liquid water. | Estimates not widely available as a global percentage of total liquid water. |
Although a precise global percentage of total liquid water is hard to estimate for brackish water, these environments are ecologically very important. Estuaries and coastal wetlands are critical habitats for many species of fish, birds, and invertebrates. They also provide valuable ecosystem services, such as filtering pollutants, protecting coastlines from erosion, and serving as nurseries for marine life. Managing these variable and often sensitive brackish water ecosystems is a significant challenge for conservation and resource management.
The difficulty in globally quantifying brackish water as a percentage of total liquid water highlights its dynamic and transitional nature compared to major water reservoirs like oceans or ice caps.
The percentage of fresh water available as polar ice/glaciers compared to total fresh water is:-
An isohyet is a line joining points of
Engineering hydrology does NOT deal with:
For one-dimensional flow without recharge in an unconfined aquifer between two water bodies, the steady water table profile is
The water balance equation for a catchment area in terms of rainfall (P), runoff (R), evaporation (E) and storage (S) is written as