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  2. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    In the aquifer, groundwater flows from points of higher pressure to points of lower pressure, and the direction of groundwater flow typically has both a horizontal and a vertical component. The slope of the water table is known as the “hydraulic gradient”, which depends on the rate at which water is added to and removed from the aquifer and ...

  3. System of Environmental and Economic Accounting for Water

    en.wikipedia.org/wiki/System_of_Environmental...

    The SEEA-Water is a conceptual framework for the organization of physical and economic information related to water using concepts, definitions and classifications consistent to those of the System of National Accounts 2008 (2008 SNA). The SEEA-Water framework is an elaboration of the handbook on Integrated Environmental and Economic Accounting ...

  4. Watertable control - Wikipedia

    en.wikipedia.org/wiki/Watertable_control

    In geotechnical engineering, watertable control is the practice of controlling the height of the water table by drainage.Its main applications are in agricultural land (to improve the crop yield using agricultural drainage systems) and in cities to manage the extensive underground infrastructure that includes the foundations of large buildings, underground transit systems, and extensive ...

  5. Groundwater banking - Wikipedia

    en.wikipedia.org/wiki/Groundwater_banking

    The banking system could then be set up to allow trading of credits. [2] There are several objectives of the water bank accounting system: track water deposits, withdrawals, and to control the amount, timing, and location of withdrawals by the participants. [2] If groundwater is not regulated there is more of a chance for freeriding and overuse ...

  6. Phreatic zone - Wikipedia

    en.wikipedia.org/wiki/Phreatic_zone

    Cross section showing the water table varying with surface topography as well as a perched water table. The phreatic zone, saturated zone, or zone of saturation, is the part of an aquifer, below the water table, in which relatively all pores and fractures are saturated with water.

  7. Groundwater recharge - Wikipedia

    en.wikipedia.org/wiki/Groundwater_recharge

    Groundwater recharge is an important process for sustainable groundwater management, since the volume-rate abstracted from an aquifer in the long term should be less than or equal to the volume-rate that is recharged. Recharge can help move excess salts that accumulate in the root zone to deeper soil layers, or into the groundwater system.

  8. Groundwater-dependent ecosystems - Wikipedia

    en.wikipedia.org/wiki/Groundwater-dependent...

    Graphic on Groundwater Flow. Groundwater-Dependent Ecosystems (or GDEs) are ecosystems that rely upon groundwater for their continued existence. Groundwater is water that has seeped down beneath Earth's surface and has come to reside within the pore spaces in soil and fractures in rock, this process can create water tables and aquifers, which are large storehouses for groundwater.

  9. Chart of accounts - Wikipedia

    en.wikipedia.org/wiki/Chart_of_accounts

    A chart of accounts (COA) is a list of financial accounts and reference numbers, grouped into categories, such as assets, liabilities, equity, revenue and expenses, and used for recording transactions in the organization's general ledger. Accounts may be associated with an identifier (account number) and a caption or header and are coded by ...