Ok, after talking a lot about soil, rocks and agriculture, let’s talk a little bit about water.
I guess it’s not unknown that even though water is abundant, the water that we can drink is quire rare. If 97,5% of Earth’s water resides in the oceans and is too salty to drink or use to water crops, than it lasts only 2,5% of the type considered fresh, which is water with few dissolved salts. Since most fresh water is tied up in calaciers, icecaps, and underground aquifers, just over 1 part in 10,000 of Earth’s water is easily accessible for human use.
Water constantly moves via the hydrologic cycle and, as it moves, it redistributes heat, erodes mountain ranges, builds river deltas, maintains organisms and ecosystems, shapes civilizations, and gives rise to political conflicts.
The freshwater ecosystems are rich in life, and they are:
- Rivers and streams – water from rain, snowmelt,or springs runs downhill and converges where the land dips lowest, forming streams, creeks, or brooks. These water-courses merge into rivers;
- Lakes and ponds – bodies of open standing water. Their physical conditions and the types of life within them vary with depth and the distance from shore.
- Marshes, swamps, and bogs – systems that combine elements of fresh water and dry land. They’re also called wetlands, and are very rich and productive.
Groundwater is very important to the hydrologic cycle because the precipitation that reach Earth’s land surface and does not evaporate, flow into waterways, or get taken up by organisms infiltrates the surface. Most percolates downward through the soil to become groundwater.
Groundwater is contained within aquifers, porous, spongelike formations of rock, sand, or gravel that hold water. The world’s largest known aquifer is the Ogallala Aquifer, which underlines the Great Plains beneath eight US states from South Dakota to Texas. However, overpumping for irrigation has reduced this aquifer’s volume by nearly 10% so far -a volume equal to 18 years’worth of the entire flow of the Coloado River.
Unfortunatelly for us, different regions of the world possess vastly different amounts of groundwater, surface water, and precipitation. However, people are not distributed across the globe in accordance with water availability. Canada, for instance, has 20 times more water per citizan than does China; the Amazon River carries 15% of the world’s runoff, but its watershed holds less than half a percent of the world’s population. Many countries like Pakistan, Iran and Egypt face water shortages.
Because fresh water is distributed unevenly in time and space, it became necessary to erect dams to store water, so that it may be distributed when needed. In India, monsoon storms can dump half of a region’s annual rain in just a few hours. Northwest China receivs three-fifths of its annual precipitation during 3 months, when crops do not need it.
We divert and deplete surface wter to suit our needs. Water from rivers, streams, lakes and ponds are diverted to homes, cities, and farm fields. The Colorado River’s water, for instance, is heavily diverted and utilized, in a way that after all the diversions comprised, just a trickle makes its way to the Gulf of California. There are some days when water does not reach the Gulf at all. This flow reduction has altered drastically the river and its once rich delta; plant communities were modified and populations of fish and aquatic invertebrates where wipped out, devastating fisheries.
We are depleting groundwater more than surface water because most aquifers recharge very slowly. Most groundwater use goes toward agriculure. We withdraw 70% more water for irrigation today than in 1960, and since then, the amount of land under irrigation has doubled. Expansion of irrigated agriculture has kept pace with population growth. Irrigation can more than double crop yields by allowing farmers to apply water when and where it is needed. Still, most irrigation remains inefficient, and overirrigatin leads to waterlogging and salinization.
Worldwide today, 15-35% of irrigation withdrawals are thought to be unsustainable, and like Ogallala, many aquifers are being drained as water is “mined” at rates faster than it is recharged. As aquifers are depleted, water tables drop. Groundwater becomes more difficult and expensive to extract, and eventually it may run out. To make the situation even worse, when groundwater is overpumped in coastal areas, salt water can intrude into aquifers, making water undrinkable; and as aquifers lose water, the land surface aboe may subside, that’s the reason why cities from Venice to Bangkok to Mexico City are slowly sinking, while streets buckle, buildings flood, and pipes break.
Still, there are some solutions to depletion of fresh water:
- To address the depletion, we can aim either to increase supply or to reduce demand, lowering demand is more difficult politically but will likely be necessary in the long term;
- To increase supply in a giver area, people have transported water through pipes and aqueducts from areas where it is more plentiful or accessible. In many instances, water-poor regions have forcibly appopriated water from commmunities too weak to keep it for themselves. Los Angeles, for instance, grew by using water it appropriated from the Owens Valley, Mono Lake, and other rural regions of California. Becaouse of that, these area’s environments are desertified, crating dustbowls and devastating local economies.
- Desalination also may help. The process of “making” fresh water by removing salt from seawater or other water of marginal quality. However, desalination is expensve, requires large inputs of fossil fuel energy, and generates concentrated salty waste. Over 7,500 desalination facilities are operating worldwide. Most are in the Middle East, where water is scarce and oil is cheap.
- To decrease demand farmers can improve efficiency by lining irrigation canals to prevent leaks, leveling fields to minimize runoff, and adopting efficient irrigation methods.
- Choosing crops to match the land and climate in which they are being farmed can save huge amounts of water. Crops that require a great deal of water are cotton, rice and alfalfa are often planted in arid areas with government-subsidized irrigation. In this way, the true cost of water is not part of the cost of growing the crop.











