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Water resources

Sources of water that are potentially useful for humans

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Water resources are under threat from multiple issues. There is water scarcity, water pollution, water conflict, and climate change. Fresh water is in principle a renewable resource. However, the world's supply of groundwater is steadily decreasing. Groundwater depletion (or overdrafting) is occurring for example in Asia, South America and North America.

Natural sources of fresh water

Natural sources of fresh water include surface water, under river flow, groundwater and frozen water.

Surface water

Surface water refers to water that is found on the surface of the Earth. This includes but not limited to river, lake, ponds or fresh water wetland. Surface water is naturally replenished by precipitation, and naturally lost through discharge to the oceans, evaporation, evapotranspiration, drought, climate change, population growth, deforestation, land degradation, and groundwater recharge. The only natural input to any surface water system is precipitation within its watershed. The total quantity of water in that system at any given time is also dependent on many other factors. These factors include storage capacity in lakes, wetlands and artificial reservoirs, the permeability of the soil beneath these storage bodies, the runoff characteristics of the land in the watershed, the timing of the precipitation and local evaporation rates. Furthermore, other human factors such as temperature, climate change, topography, Vegetation cover, windspeed, relative humidity, and solar radiation has an effect on water loss. All of these factors also affect the proportions of water loss.

Humans often increase storage capacity by constructing reservoirs, rainwater harvesting systems, Managed Aquifier Recharge (MAR), Watershed Conservation, Construction of retention, and detention basins, floodplain restoration, creation of artificial rains; and decrease it by draining wetlands, land reclamation, urbanisation, river channelisation, over-abstraction of water, sedimentation by deforestation and poor reservoir management. Humans often increase runoff quantities and velocities by paving areas and channelizing the stream flow.

Natural surface water can be augmented by importing surface water from another watershed through a canal or pipeline. Other methods also includes rain harvesting, construction of dams and reservoirs, desalination, cloud seeding, and artificial recharge.

Brazil is estimated to have the largest supply of fresh water in the world with 5,661 billion m³/year followed by Russia, and Canada, with about 4,312 billion m³/year and 2,850 billion m³/year respectively according to rècent World Bank summaries. However, this is renewable freshwater and not freshwater physically stored in lakes,groundwater or glaciers.

Water from glaciers

Glacier runoff is considered to be surface water. The Himalayas, which are often called "The Roof of the World", contain some of the most extensive and rough high altitude areas on Earth as well as the greatest area of glaciers and permafrost outside of the poles. Ten of Asia's largest rivers flow from there, and more than a billion people's livelihoods depend on them. To complicate matters, temperatures there are rising more rapidly than the global average. In Nepal, the temperature has risen by 0.6 degrees Celsius over the last decade, whereas globally, the Earth has warmed approximately 0.7 degrees Celsius over the last hundred years.

Groundwater

Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available fresh water in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology.

Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, permafrost (frozen soil), immobile water in very low permeability bedrock, and deep geothermal or oil formation water. Groundwater is hypothesized to provide lubrication that can possibly influence the movement of faults. It is likely that much of Earth's subsurface contains some water, which may be mixed with other fluids in some instances.

Under river flow

Throughout the course of a river, the total volume of water transported downstream will often be a combination of the visible free water flow together with a substantial contribution flowing through rocks and sediments that underlie the river and its floodplain called the hyporheic zone. For many rivers in large valleys, this unseen component of flow may greatly exceed the visible flow. The hyporheic zone often forms a dynamic interface between surface water and groundwater from aquifers, exchanging flow between rivers and aquifers that may be fully charged or depleted. This is especially significant in karst areas where pot-holes and underground rivers are common.

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