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The state used 38 billion gallons of water a day in 2010, which works out to around 1.3 trillion gallons a year.
A growing agricultural sector in the state, combined with persistent drought, has only increased the demand for water, and traditional sources of groundwater haven’t kept up with the state’s thirst. Many of the underground aquifers are at risk of being contaminated by oil and gas drilling activities in the region.
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When dirty water from the wells is forced back into the ground, it causes pressure increases that can allow run-off to spread via faults throughout the bedrock.
While most oil wells are deep, if the pressure is sufficient, it will push the water back upwards, toward untouched reserves of fresh water.
When the water is pumped out, what was previously a pool becomes an empty cavern, and if the surrounding rock isn’t stable enough, it can buckle inwards.
It’s quite similar to the process that leads to sinkholes, and can similarly lead to major problems for buildings and infrastructure on the surface.
While the survey extended to around 10,000 feet, the researchers say that much of the water lies closer to the surface, around 3,000 feet deep.
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The dual challenges of extracting and treating the water are indications that these underground aquifers may not be the bonanza they seem to be.
It is clear however, that California must adapt to a drier future, whether that means tapping new sources of water or cutting back consumption.