Groundwater recharge

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Water balance

Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface. Groundwater recharge also encompasses water moving away from the water table farther into the saturated zone.[1] Recharge occurs both naturally (through the water cycle) and through anthropogenic processes (i.e., "artificial groundwater recharge"), where rainwater and/or reclaimed water is routed to the subsurface.

The most common methods to estimate recharge rates are: chloride mass balance (CMB); soil physics methods; environmental and isotopic tracers; groundwater-level fluctuation methods; water balance (WB) methods (including groundwater models (GMs)); and the estimation of baseflow (BF) to rivers.[2]

Processes

Diffused or focused mechanisms

Groundwater recharge can occur through diffuse or focused mechanisms. Diffuse recharge occurs when precipitation infiltrates through the soil to the water table, and is by definition distributed over large areas. Focused recharge occurs where water leaks from surface water sources (rivers, lakes, wadis, wetlands) or land surface depressions, and generally becomes more dominant with aridity.[2]

Natural recharge

Natural processes of groundwater recharge. Adjustments affecting the water table will drastically enhance or diminish the quality of groundwater recharge in a specific region.

Water is recharged naturally by

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. Tree roots increase water

permeability by moving clay soils downstream, and this increases aquifer recharge.[4]

Wetlands

Wetlands help maintain the level of the water table and exert control on the hydraulic head.[5][6] This provides force for groundwater recharge and discharge to other waters as well. The extent of groundwater recharge by a wetland is dependent upon soil, vegetation, site, perimeter to volume ratio, and water table gradient.[7][8] Groundwater recharge occurs through mineral soils found primarily around the edges of wetlands.[9] The soil under most wetlands is relatively impermeable. A high perimeter to volume ratio, such as in small wetlands, means that the surface area through which water can infiltrate into the groundwater is high.[8] Groundwater recharge is typical in small wetlands such as prairie potholes, which can contribute significantly to recharge of regional groundwater resources.[8] Researchers have discovered groundwater recharge of up to 20% of wetland volume per season.[8]

Artificial groundwater recharge

Managed aquifer recharge (MAR) strategies to augment freshwater availability include streambed channel modification, bank filtration, water spreading and recharge wells.[10]: 110  A facility in Orange County, California cleans and injects 100 million gallons per day;[11] or 90 billion gallons per year.[12]

Artificial groundwater recharge is becoming increasingly important in India, where over-pumping of groundwater by farmers has led to underground resources becoming depleted. In 2007, on the recommendations of the International Water Management Institute, the Indian government allocated ₹1,800 crore (equivalent to ₹54 billion or US$630 million in 2023) to fund dug-well recharge projects (a dug-well is a wide, shallow well, often lined with concrete) in 100 districts within seven states where water stored in hard-rock aquifers had been over-exploited. Another environmental issue is the disposal of waste through the water flux such as dairy farms, industrial, and urban runoff.

Pollution in stormwater

retention ponds and rain gardens
.

Depression-focused recharge

If water falls uniformly over a field such that field capacity of the soil is not exceeded, then negligible water percolates to groundwater. If instead water puddles in low-lying areas, the same water volume concentrated over a smaller area may exceed field capacity resulting in water that percolates down to recharge groundwater. The larger the relative contributing runoff area is, the more focused infiltration is. The recurring process of water that falls relatively uniformly over an area, flowing to groundwater selectively under surface depressions is depression focused recharge. Water tables rise under such depressions.

Depression focused groundwater recharge can be very important in

arid regions
. More rain events are capable of contributing to groundwater supply.

Depression focused groundwater recharge also profoundly effects

contaminant transport into groundwater. This is of great concern in regions with karst geological formations because water can eventually dissolve tunnels all the way to aquifers, or otherwise disconnected streams. This extreme form of preferential flow, accelerates the transport of contaminants and the erosion of such tunnels. In this way depressions intended to trap runoff water—before it flows to vulnerable water resources—can connect underground over time. Cavitation of surfaces above into the tunnels, results in potholes
or caves.

Deeper ponding exerts pressure that forces water into the ground faster. Faster flow dislodges contaminants otherwise adsorbed on soil and carries them along. This can carry pollution directly to the raised water table below and into the groundwater supply. Thus, the quality of water collecting in infiltration basins is of special concern.

Estimation methods

Rates of groundwater recharge are difficult to quantify.[13][2] This is because other related processes, such as evaporation, transpiration (or evapotranspiration) and infiltration processes must first be measured or estimated to determine the balance. There are no widely applicable method available that can directly and accurately quantify the volume of rainwater that reaches the water table.[2]

The most common methods to estimate recharge rates are: chloride mass balance (CMB); soil physics methods; environmental and isotopic tracers; groundwater-level fluctuation methods; water balance (WB) methods (including groundwater models (GMs)); and the estimation of baseflow (BF) to rivers.[2]

Regional, continental and global estimates of recharge commonly derive from global hydrological models.[2]

Physical

Physical methods use the principles of soil physics to estimate recharge. The direct physical methods are those that attempt to actually measure the volume of water passing below the root zone. Indirect physical methods rely on the measurement or estimation of soil physical parameters, which along with soil physical principles, can be used to estimate the potential or actual recharge. After months without rain the level of the rivers under humid climate is low and represents solely drained groundwater. Thus, the recharge can be calculated from this base flow if the catchment area is already known.

Chemical

Chemical methods use the presence of relatively

isotopic tracer[14][15][16] or chloride,[17]
moving through the soil, as deep drainage occurs.

Numerical models

Recharge can be estimated using

WEAP, and MIKE SHE. The 1D-program HYDRUS1D is available online. The codes generally use climate and soil data to arrive at a recharge estimate and use the Richards equation in some form to model groundwater flow in the vadose zone
.

Factors affecting groundwater recharge

Climate change

See also: Effects of climate change on the water cycle
This section is an excerpt from Groundwater § Climate change.[edit]

The impacts of climate change on groundwater may be greatest through its indirect effects on irrigation water demand via increased evapotranspiration.[18]: 5  There is an observed declined in groundwater storage in many parts of the world. This is due to more groundwater being used for irrigation activities in agriculture, particularly in drylands.[19]: 1091  Some of this increase in irrigation can be due to water scarcity issues made worse by effects of climate change on the water cycle. Direct redistribution of water by human activities amounting to ~24,000 km3 per year is about double the global groundwater recharge each year.[19]

Climate change causes changes to the water cycle which in turn affect groundwater in several ways: There can be a decline in groundwater storage, and reduction in groundwater recharge and water quality deterioration due to extreme weather events.[20]: 558  In the tropics intense precipitation and flooding events appear to lead to more groundwater recharge.[20]: 582 

However, the exact impacts of climate change on groundwater are still under investigation.[20]: 579  This is because scientific data derived from groundwater monitoring is still missing, such as changes in space and time, abstraction data and "numerical representations of groundwater recharge processes".[20]: 579 

Effects of climate change could have different impacts on groundwater storage: The expected more intense (but fewer) major rainfall events could lead to increased groundwater recharge in many environments.[18]: 104  But more intense drought periods could result in soil drying-out and compaction which would reduce infiltration to groundwater.[21]

Urbanization

Further implications of groundwater recharge are a consequence of

permeable compared to soil, resulting in higher amounts of surface runoff. Therefore, urbanization increases the rate of groundwater recharge and reduces infiltration,[23]
resulting in flash floods as the local ecosystem accommodates changes to the surrounding environment.

Adverse factors

See also

References

  1. OCLC 643719314. Accessed from: http://hydrogeologistswithoutborders.org/wordpress/1979-english/ Archived 2020-04-06 at the Wayback Machine
  2. ^
    S2CID 233941479. Text was copied from this source, which is available under a Creative Commons Attribution 4.0 International License
  3. ^ "Urban Trees Enhance Water Infiltration". Fisher, Madeline. The American Society of Agronomy. November 17, 2008. Archived from the original on June 2, 2013. Retrieved October 31, 2012.
  4. ^ "Major floods recharge aquifers". University of New South Wales. January 24, 2011. Retrieved October 31, 2012.
  5. ^ O'Brien 1988
  6. S2CID 102489854
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  7. ISBN 978-1-4684-8378-9
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  8. ^
    OCLC 476093538
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  9. JSTOR 1938872
    .
  10. ^ United Nations (2022) The United Nations World Water Development Report 2022: Groundwater: Making the invisible visible. UNESCO, Paris Text was copied from this source, which is available under a Creative Commons Attribution 3.0 International License
  11. ^ "Groundwater Replenishment System (GWRS), Orange County, California - Water Technology". www.water-technology.net.
  12. ^ "Orange County Water District achieves record year of groundwater recharge". Smart Water Magazine. 19 August 2024.
  13. S2CID 39943677
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  14. ISSN 0084-6597
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  15. S2CID 155563380
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  16. S2CID 219743798
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  17. doi:10.1071/SR9780181
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  18. ^ a b United Nations (2022) The United Nations World Water Development Report 2022: Groundwater: Making the invisible visible. UNESCO, Paris Text was copied from this source, which is available under a Creative Commons Attribution 3.0 International License
  19. ^
    ISBN 978-1-009-15789-6. {{cite book}}: no-break space character in |first11= at position 3 (help); no-break space character in |first12= at position 3 (help); no-break space character in |first13= at position 3 (help); no-break space character in |first14= at position 3 (help
    )
  20. ^
    ISBN 978-1-009-32584-4
    .
  21. ^ IAH (2019). "Climate-Change Adaptation & Groundwater" (PDF). Strategic Overview Series.
  22. ^ a b "Groundwater depletion". USGS Water Science School. United States Geological Survey. 2016-12-09.
  23. ^ a b "Effects of Urban Development on Floods". pubs.usgs.gov. Retrieved 2019-03-22.


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