
CHAPTER 5 The impact of aquifer intensive use on groundwater
... Natural groundwater quality is also frequently affected by the excessive content of minor constituents, particularly by iron, manganese, fluorine and iodine. Iron content is common in groundwater. Drinking water standards in many countries tolerate an iron content within 0.3 mg/L. The amount of oxyg ...
... Natural groundwater quality is also frequently affected by the excessive content of minor constituents, particularly by iron, manganese, fluorine and iodine. Iron content is common in groundwater. Drinking water standards in many countries tolerate an iron content within 0.3 mg/L. The amount of oxyg ...
Deloitte Access Economics - National Centre for Groundwater
... Current average annual groundwater use is approximately 3,500 GL. Groundwater is used across many industries of the Australian economy. Water used for agricultural irrigation is the largest single user group, comprising on average approximately 60% of Australia’s annual groundwater use. Other user g ...
... Current average annual groundwater use is approximately 3,500 GL. Groundwater is used across many industries of the Australian economy. Water used for agricultural irrigation is the largest single user group, comprising on average approximately 60% of Australia’s annual groundwater use. Other user g ...
CHAPTER 17 Intensive use of groundwater in some areas of China
... to the sea is more than 300 km and precipitation is about one third of that in Japan, it is not possible for freshwater to discharge directly into the sea, and its salinity rises even in the inland side from the coast and salt accumulation has generated. Those regions are economically important plac ...
... to the sea is more than 300 km and precipitation is about one third of that in Japan, it is not possible for freshwater to discharge directly into the sea, and its salinity rises even in the inland side from the coast and salt accumulation has generated. Those regions are economically important plac ...
Characterization of Groundwater Systems - AGW-Net
... current long-term average rate of aquifer recharge, although should also consider: value judgements about the importance of maintaining some of the natural discharges from the aquifer system consideration of consumptive use and catchment export, as opposed to local non-consumptive uses which resul ...
... current long-term average rate of aquifer recharge, although should also consider: value judgements about the importance of maintaining some of the natural discharges from the aquifer system consideration of consumptive use and catchment export, as opposed to local non-consumptive uses which resul ...
Appendix 1: Agricultural water wells in Canada
... caused by local point source pollution such as livestock effluents, mining, other industries, and waste disposal; it may also be caused regionally by diffuse sources such as agriculture. The National Water Research Institute (NWRI) and the Geological Survey of Canada (GSC) are collecting information ...
... caused by local point source pollution such as livestock effluents, mining, other industries, and waste disposal; it may also be caused regionally by diffuse sources such as agriculture. The National Water Research Institute (NWRI) and the Geological Survey of Canada (GSC) are collecting information ...
Water scarcity - Topping Geography
... Kazakhstan and Uzbekistan. The Aral Sea used to be the fourth largest inland lake in the world, with a surface area of 68,000km2. The sea is fed by two rivers, the Amu Darya and the Syr Darya. Since the 1960's the sea has been shrinking because they were diverted by USSR to irrigate the desert to in ...
... Kazakhstan and Uzbekistan. The Aral Sea used to be the fourth largest inland lake in the world, with a surface area of 68,000km2. The sea is fed by two rivers, the Amu Darya and the Syr Darya. Since the 1960's the sea has been shrinking because they were diverted by USSR to irrigate the desert to in ...
Water scarcity

Water scarcity is the lack of sufficient available water resources to meet the demands of water usage within a region. It already affects every continent and around 2.8 billion people around the world at least one month out of every year. More than 1.2 billion people lack access to clean drinking water.Water scarcity involves water stress, water shortage or deficits, and water crisis. While the concept of water stress is relatively new, it is the difficulty of obtaining sources of fresh water for use during a period of time and may result in further depletion and deterioration of available water resources. Water shortages may be caused by climate change, such as altered weather patterns including droughts or floods, increased pollution, and increased human demand and overuse of water. A water crisis is a situation where the available potable, unpolluted water within a region is less than that region's demand. Water scarcity is being driven by two converging phenomena: growing freshwater use and depletion of usable freshwater resources.Water scarcity can be a result of two mechanisms: physical (absolute) water scarcity and economic water scarcity, where physical water scarcity is a result of inadequate natural water resources to supply a region's demand, and economic water scarcity is a result of poor management of the sufficient available water resources. According to the United Nations Development Programme, the latter is found more often to be the cause of countries or regions experiencing water scarcity, as most countries or regions have enough water to meet household, industrial, agricultural, and environmental needs, but lack the means to provide it in an accessible manner.The reduction of water scarcity is a goal of many countries and governments. The UN recognizes the importance of reducing the number of people without sustainable access to clean water and sanitation. The Millennium Development Goals within the United Nations Millennium Declaration state that by 2015 they resolve to ""halve the proportion of people who are unable to reach or to afford safe drinking water.""