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Groundwater recharge

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397:. 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 133: 3533: 2992: 222: 36: 726: 678:
surface water from percolating into the soil, resulting in most surface runoff entering storm drains for local water supply. As urban development continues to spread across various regions, rates of groundwater recharge will increase relative to the existing rates of the previous rural region. A consequence of sudden influxes in groundwater recharge includes
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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. In the tropics intense precipitation and flooding events appear to lead to more groundwater recharge.
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This is explained through the vast water supply and sewage networks supported in urban regions in which rural areas are not likely to obtain. Recharge in rural areas is heavily supported by precipitation and this is opposite for urban areas. Road networks and infrastructure within cities prevents
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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,
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However, the exact impacts of climate change on groundwater are still under investigation. 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".
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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.
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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.
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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
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compared to soil, resulting in higher amounts of surface runoff. Therefore, urbanization increases the rate of groundwater recharge and reduces infiltration, resulting in flash floods as the local ecosystem accommodates changes to the surrounding environment.
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found primarily aro. 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 typical in small wetlands such as
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MacDonald, Alan M; Lark, R Murray; Taylor, Richard G; Abiye, Tamiru; Fallas, Helen C; Favreau, Guillaume; Goni, Ibrahim B; Kebede, Seifu; Scanlon, Bridget; Sorensen, James P R; Tijani, Moshood; Upton, Kirsty A; West, Charles (2021-03-01).
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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.
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Douville, H.; Raghavan, K.; Renwick, J.; Allan, R.P.; Arias, P.A.; Barlow, M.; Cerezo-Mota, R.; Cherchi, A.; Gan, T.Y.; Gergis, J.; Jiang, D.; Khan, A.; Pokam Mba, W.; Rosenfeld, D.; Tierney, J.; Zolina, O. (2021).
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help maintain the level of the water table he hydraulic head. This provides force for groundwater recharge and discharge to other waters as well. The extent of groundwater recharge by a wetland is dependent upon
2022: 623:. 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 1650: 320:, which can contribute significantly to recharge of regional groundwater resources. Researchers have discovered groundwater recharge of up to 20% of wetland volume per season. 225:
Natural processes of groundwater recharge. Adjustments affecting the water table will drastically enhance or diminish the quality of groundwater recharge in a specific region.
1528:. In Pörtner, H.-O.; Roberts, D.C.; Tignor, M.; Poloczanska, E.S.; Mintenbeck, K.; Alegría, A.; Craig, M.; Langsdorf, S.; Löschke, S.; Möller, V.; Okem, A.; Rama, B. (eds.). 1521:
Caretta, M.A.; Mukherji, A.; Arfanuzzaman, M.; Betts, R.A.; Gelfan, A.; Hirabayashi, Y.; Lissner, T.K.; Liu, J.; Lopez Gunn, E.; Morgan, R.; Mwanga, S.; Supratid, S. (2022).
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Climate Change 2022: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
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surface. Groundwater recharge also encompasses water moving away from the water table farther into the saturated zone. Recharge occurs both naturally (through the
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Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
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melt and to a smaller extent by surface water (rivers and lakes). Recharge may be impeded somewhat by human activities including paving, development, or
3422: 635:. Direct redistribution of water by human activities amounting to ~24,000 km per year is about double the global groundwater recharge each year. 268:
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
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that forces water into the ground faster. Faster flow dislodges contaminants otherwise adsorbed on soil and carries them along. This can carry
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Allison, G.B.; Hughes, M.W. (1978). "The use of environmental chloride and tritium to estimate total recharge to an unconfined aquifer".
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groundwater recharge in many environments. But more intense drought periods could result in soil drying-out and compaction which would
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Reilly, Thomas E.; LaBaugh, James W.; Healy, Richard W.; Alley, William M. (2002-06-14). "Flow and Storage in Groundwater Systems".
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The impacts of climate change on groundwater may be greatest through its indirect effects on irrigation water demand via increased
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could have different impacts on groundwater storage: The expected more intense (but fewer) major rainfall events could lead to
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Winter, T.C. (1988). "A conceptual framework for assessing cumulative impacts on the hydrology of nontidal wetlands".
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of groundwater by farmers has led to underground resources becoming depleted. In 2007, on the recommendations of the
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groundwater. Thus, the recharge can be calculated from this base flow if the catchment area is already known.
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physical methods are those that attempt to actually measure the volume of water passing below the root zone.
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Rates of groundwater recharge are difficult to quantify. This is because other related processes, such as
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Managed aquifer recharge (MAR) strategies to augment freshwater availability include streambed. channel
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Carter, V.; Novitzki, R.P. (1988). "Some Comments on the Relation between Ground Water and Wetlands".
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The United Nations World Water Development Report 2022: Groundwater: Making the invisible visible
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The United Nations World Water Development Report 2022: Groundwater: Making the invisible visible
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wadis, wetlands) or land surface depressions, and generally becomes more dominant with aridity.
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water—before it flows to vulnerable water resources—can connect underground over time.
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in the long term should be less than or equal to the volume-rate that is recharged.
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Regional, continental and global estimates of recharge commonly derive from global
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geological formations because water can eventually dissolve tunnels all the way to
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Artificial groundwater recharge is becoming increasingly important in India, where
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54 billion or US$ 650 million in 2023) to fund dug-well
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by moving clay soils downstream, and this increases aquifer recharge.
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transport into groundwater. This is of great concern in regions with
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Further implications of groundwater recharge are a consequence of
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Depression focused groundwater recharge can be very important in
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of the soil is not exceeded, then negligible water percolates to
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http://hydrogeologistswithoutborders.org/wordpress/1979-english/
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Depression focused groundwater recharge also profoundly effects
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Stahl, Mason O.; Gehring, Jaclyn; Jameel, Yusuf (2020-07-30).
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and reduction in recharge. Use of groundwater, especially for
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Text was copied from this source, which is available under a
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Text was copied from this source, which is available under a
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Text was copied from this source, which is available under a
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Creative Commons Attribution 3.0 International License
1261:"Oxygen and Hydrogen Isotopes in the Hydrologic Cycle" 1197:
Creative Commons Attribution 3.0 International License
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Creative Commons Attribution 4.0 International License
627:. Some of this increase in irrigation can be due to 543:, moving through the soil, as deep drainage occurs. 3441: 3268: 3190: 3044: 2927: 2785: 2666: 2526: 2517: 2327: 2122: 2035: 2005: 1954: 1945: 1889: 1852: 1826: 1788: 1755: 1707: 1664: 1104:
Freshwater Marshes: Ecology and Wildlife Management
60:. Unsourced material may be challenged and removed. 1485:. Cambridge University Press. pp. 1055–1210. 583:data to arrive at a recharge estimate and use the 245:resulting in reduced water infiltration, enhanced 462:supply. Thus, the quality of water collecting in 1534:. Cambridge University Press. pp. 551–712. 531:Chemical methods use the presence of relatively 389:If water falls uniformly over a field such that 1107:(3rd ed.). University of Minnesota Press. 439:of surfaces above into the tunnels, results in 1591:. United States Geological Survey. 2016-12-09. 587:in some form to model groundwater flow in the 257:groundwater management, since the volume-rate 3022: 1923: 1644: 1565:"Climate-Change Adaptation & Groundwater" 1265:Annual Review of Earth and Planetary Sciences 575:is available online. The codes generally use 561:Hydrologic Evaluation of Landfill Performance 8: 633:effects of climate change on the water cycle 606:Effects of climate change on the water cycle 401:. Water tables rise under such depressions. 431:. In this way depressions intended to trap 3029: 3015: 3007: 2789: 2523: 1951: 1930: 1916: 1908: 1651: 1637: 1629: 1096: 1094: 1092: 1882:: Saltmod coupled to a groundwater model 1067:. Vol. 1. Springer. pp. 68–86. 918: 241:. These activities can result in loss of 120:Learn how and when to remove this message 1606:"Effects of Urban Development on Floods" 960:"Urban Trees Enhance Water Infiltration" 337:International Water Management Institute 827: 510:Physical methods use the principles of 1065:The Ecology and Management of Wetlands 595:Factors affecting groundwater recharge 1600: 1598: 1579: 1577: 1185:="WWDR2022">United Nations (2022) 638:Climate change causes changes to the 535:water-soluble substances, such as an 171:. This process usually occurs in the 27:Groundwater that recharges an aquifer 7: 1308:"Global Isotope Hydrogeology―Review" 887: 885: 883: 881: 879: 877: 58:adding citations to reliable sources 1418:Australian Journal of Soil Research 835:Freeze, R.A.; Cherry, J.A. (1979). 3418:Ultraviolet germicidal irradiation 1306:Jasechko, Scott (September 2019). 775:Groundwater recharge in California 339:, the Indian government allocated 25: 3288:Agricultural wastewater treatment 992:. University of. January 24, 2011 289:Permeability (earth scieeability) 3532: 3531: 2991: 2990: 1699:Irrigation environmental impacts 1450: 1190: 990:"Major floods recharge aquifers" 941: 724: 611:This section is an excerpt from 551:Recharge can be estimated using 229:Water is recharged naturally by 34: 3348:Industrial wastewater treatment 3318:Decentralized wastewater system 324:Artificial groundwater recharge 45:needs additional citations for 1285:10.1146/annurev.earth.24.1.225 899:Environmental Research Letters 208:Diffused or focused mechanisms 1: 3368:Rotating biological contactor 1732:Drainage system (agriculture) 1659:Agricultural water management 790:International trade and water 195:is routed to the subsurface. 1956:Pollution / quality 1775:Hydrological transport model 1570:. Strategic Overview Series. 740:Aquifer storage and recovery 660:infiltration to groundwater. 613:Groundwater § Climate change 179:and is often expressed as a 1073:10.1007/978-1-4684-8378-9_7 755:Depression focused recharge 399:depression focused recharge 385:Depression-focused recharge 3640: 3619:Water resources management 3433:Wastewater treatment plant 3200:Adsorbable organic halides 1803:Groundwater energy balance 610: 603: 514:to estimate recharge. The 3609:Water and the environment 3527: 3205:Biochemical oxygen demand 2986: 2792: 2527:Types / location 1853:Agro-hydro-salinity group 1589:USGS Water Science School 1540:10.1017/9781009325844.006 1491:10.1017/9781009157896.010 650:Effects of climate change 3604:Sustainable technologies 1880:SahysMod polygonal model 1875:SaltMod integrated model 1780:Runoff model (reservoir) 1022:Environmental Management 920:10.1088/1748-9326/abd661 785:Infiltration (hydrology) 357:Pollution in stormwater 3393:Sewage sludge treatment 3333:Fecal sludge management 3293:API oil–water separator 3260:Wastewater surveillance 1860:Hydrology (agriculture) 1585:"Groundwater depletion" 1474:"8 Water Cycle Changes" 1259:Gat, J. R. (May 1996). 1230:10.1126/science.1067123 1151:(5): 1456–67 /1938872. 780:Hydrology (agriculture) 770:Groundwater remediation 466:is of special concern. 454:directly to the raised 3250:Total suspended solids 3245:Total dissolved solids 3210:Chemical oxygen demand 1813:Hydraulic conductivity 1445:United Nations (2022) 1367:Hydrological Processes 1101:Weller, M.W. (1994) . 807:by subsurface drainage 446:Deeper ponding exerts 284:temporarily increases 226: 137: 69:"Groundwater recharge" 3599:Sustainable gardening 3569:Hydraulic engineering 3117:Industrial wastewater 1870:Leaching model (soil) 1865:Soil salinity control 1694:Irrigation management 1689:Irrigation statistics 1312:Reviews of Geophysics 805:Soil salinity control 712:Groundwater pollution 631:issues made worse by 224: 135: 3459:Groundwater recharge 2902:remnant natural area 2539:storage and recovery 2205:habitat conservation 2023:Deforestation (REDD) 1757:Surface water/runoff 1332:10.1029/2018RG000627 1136:Verry, D.R. (1982). 800:Rainwater harvesting 159:moves downward from 141:Groundwater recharge 54:improve this article 3373:Secondary treatment 3358:Membrane bioreactor 3313:Constructed wetland 3112:Infiltration/Inflow 2856:Earth Overshoot Day 2430:Marine conservation 2411:non-timber products 1834:Acid sulphate soils 1709:Subsurface drainage 1379:2020HyPr...34.3506S 1324:2019RvGeo..57..835J 1277:1996AREPS..24..225G 1222:2002Sci...296.1985A 1157:1982Ecol...63.1456V 1034:1988EnMan..12..605W 911:2021ERL....16c4012M 702:Impervious surfaces 500:hydrological models 464:infiltration basins 458:below and into the 3614:Water conservation 3594:Sustainable design 3538:Category: Sewerage 3499:Septic drain field 3464:Infiltration basin 3408:Stabilization pond 3328:Facultative lagoon 3192:Quality indicators 3072:Blackwater (waste) 3052:Acid mine drainage 2841:Ecosystem services 1964:Ambient standards 1770:Hydrological model 1737:Watertable control 1674:Surface irrigation 1042:10.1007/BF01867539 868:2020-04-06 at the 816:Watertable control 621:evapotranspiration 484:evapotranspiration 470:Estimation methods 227: 138: 3546: 3545: 3323:Extended aeration 3270:Treatment options 3220:Oxygen saturation 3067:Blackwater (coal) 3045:Sources and types 3004: 3003: 2982: 2981: 2781: 2780: 2460:genetic resources 2396:genetic resources 2031: 2030: 1939:Natural resources 1905: 1904: 1808:Groundwater model 1765:Contour trenching 1747:Drainage by wells 1742:Drainage research 1727:Drainage equation 1549:978-1-009-32584-4 1500:978-1-009-15789-6 1430:10.1071/SR9780181 1387:10.1002/hyp.13832 1373:(16): 3506–3523. 1216:(5575): 1985–90. 1114:978-0-8166-8574-5 1082:978-1-4684-8378-9 848:978-0-13-365312-0 841:. Prentice-Hall. 765:Groundwater model 750:Contour trenching 585:Richards equation 571:. The 1D-program 553:numerical methods 352:recharge projects 130: 129: 122: 104: 16:(Redirected from 3631: 3535: 3534: 3454:Evaporation pond 3442:Disposal options 3413:Trickling filter 3398:Sewage treatment 3298:Carbon filtering 3278:Activated sludge 3031: 3024: 3017: 3008: 2994: 2993: 2945: 2892:Natural heritage 2851:overexploitation 2790: 2524: 2470:herbal medicines 2450:FAO Plant Treaty 1990: 1967: 1952: 1932: 1925: 1918: 1909: 1798:Groundwater flow 1684:Tidal irrigation 1653: 1646: 1639: 1630: 1620: 1619: 1617: 1616: 1602: 1593: 1592: 1581: 1572: 1571: 1569: 1560: 1554: 1553: 1527: 1518: 1505: 1504: 1478: 1468: 1459: 1454: 1449:. UNESCO, Paris 1443: 1434: 1433: 1413: 1407: 1406: 1358: 1352: 1351: 1303: 1297: 1296: 1256: 1250: 1249: 1205: 1199: 1194: 1189:. UNESCO, Paris 1183: 1177: 1176: 1142: 1133: 1127: 1126: 1098: 1087: 1086: 1060: 1054: 1053: 1017: 1011: 1008: 1002: 1001: 999: 997: 986: 980: 979: 977: 975: 964:Fisher, Madeline 956: 950: 945: 940: 922: 889: 872: 860: 832: 734: 729: 728: 547:Numerical models 363:retention basins 349: 345: 343: 318:prairie potholes 217:Natural recharge 149:deep percolation 125: 118: 114: 111: 105: 103: 62: 38: 30: 21: 18:Aquifer recharge 3639: 3638: 3634: 3633: 3632: 3630: 3629: 3628: 3579:Land management 3549: 3548: 3547: 3542: 3523: 3489:Reclaimed water 3437: 3363:Reverse osmosis 3264: 3186: 3152:Reverse osmosis 3077:Boiler blowdown 3040: 3035: 3005: 3000: 2978: 2943: 2923: 2909:Systems ecology 2875:Natural capital 2777: 2662: 2651:reclaimed water 2513: 2475:UPOV Convention 2323: 2118: 2027: 2001: 1997:Ozone depletion 1988: 1965: 1941: 1936: 1906: 1901: 1885: 1848: 1822: 1784: 1751: 1703: 1679:Drip irrigation 1660: 1657: 1626: 1624: 1623: 1614: 1612: 1604: 1603: 1596: 1583: 1582: 1575: 1567: 1562: 1561: 1557: 1550: 1525: 1520: 1519: 1508: 1501: 1476: 1470: 1469: 1462: 1444: 1437: 1415: 1414: 1410: 1360: 1359: 1355: 1305: 1304: 1300: 1258: 1257: 1253: 1207: 1206: 1202: 1184: 1180: 1165:10.2307/1938872 1140: 1135: 1134: 1130: 1115: 1100: 1099: 1090: 1083: 1062: 1061: 1057: 1019: 1018: 1014: 1009: 1005: 995: 993: 988: 987: 983: 973: 971: 970:on June 2, 2013 958: 957: 953: 891: 890: 875: 870:Wayback Machine 861:Accessed from: 849: 834: 833: 829: 824: 811:Subsurface dyke 730: 723: 720: 707:Soil compaction 693: 691:Adverse factors 667: 662: 661: 616: 608: 602: 597: 549: 537:isotopic tracer 529: 508: 472: 387: 375:retention ponds 371:detention ponds 347: 346:(equivalent to 341: 340: 326: 297: 276:reducing water 219: 210: 205: 193:reclaimed water 155:process, where 126: 115: 109: 106: 63: 61: 51: 39: 28: 23: 22: 15: 12: 11: 5: 3637: 3635: 3627: 3626: 3621: 3616: 3611: 3606: 3601: 3596: 3591: 3586: 3581: 3576: 3571: 3566: 3564:Soil mechanics 3561: 3551: 3550: 3544: 3543: 3541: 3540: 3528: 3525: 3524: 3522: 3521: 3516: 3514:Surface runoff 3511: 3506: 3501: 3496: 3494:Sanitary sewer 3491: 3486: 3484:Marine outfall 3481: 3479:Marine dumping 3476: 3471: 3469:Injection well 3466: 3461: 3456: 3451: 3449:Combined sewer 3445: 3443: 3439: 3438: 3436: 3435: 3430: 3425: 3420: 3415: 3410: 3405: 3400: 3395: 3390: 3388:Settling basin 3385: 3380: 3375: 3370: 3365: 3360: 3355: 3350: 3345: 3340: 3335: 3330: 3325: 3320: 3315: 3310: 3305: 3300: 3295: 3290: 3285: 3283:Aerated lagoon 3280: 3274: 3272: 3266: 3265: 3263: 3262: 3257: 3252: 3247: 3242: 3237: 3232: 3227: 3222: 3217: 3215:Coliform index 3212: 3207: 3202: 3196: 3194: 3188: 3187: 3185: 3184: 3179: 3174: 3169: 3164: 3159: 3157:Sanitary sewer 3154: 3149: 3144: 3142:Produced water 3139: 3134: 3129: 3124: 3119: 3114: 3109: 3104: 3099: 3094: 3089: 3087:Combined sewer 3084: 3079: 3074: 3069: 3064: 3059: 3054: 3048: 3046: 3042: 3041: 3036: 3034: 3033: 3026: 3019: 3011: 3002: 3001: 2999: 2998: 2987: 2984: 2983: 2980: 2979: 2977: 2976: 2967: 2962: 2957: 2952: 2947: 2944:(perpetuation) 2939: 2933: 2931: 2925: 2924: 2922: 2921: 2916: 2911: 2906: 2905: 2904: 2897:Nature reserve 2894: 2889: 2888: 2887: 2882: 2872: 2871: 2870: 2860: 2859: 2858: 2853: 2843: 2838: 2837: 2836: 2831: 2821: 2820: 2819: 2814: 2809: 2804: 2793: 2787: 2783: 2782: 2779: 2778: 2776: 2775: 2774: 2773: 2768: 2758: 2753: 2748: 2743: 2738: 2733: 2728: 2723: 2718: 2713: 2708: 2703: 2702: 2701: 2691: 2686: 2681: 2676: 2670: 2668: 2664: 2663: 2661: 2660: 2655: 2654: 2653: 2643: 2638: 2633: 2632: 2631: 2621: 2616: 2615: 2614: 2602: 2601: 2600: 2595: 2590: 2580: 2575: 2574: 2573: 2568: 2563: 2553: 2548: 2543: 2542: 2541: 2530: 2528: 2521: 2515: 2514: 2512: 2511: 2510: 2509: 2504: 2494: 2489: 2484: 2483: 2482: 2477: 2472: 2467: 2462: 2457: 2452: 2442: 2437: 2432: 2427: 2426: 2425: 2415: 2414: 2413: 2408: 2403: 2398: 2388: 2387: 2386: 2381: 2376: 2374:climate change 2366: 2361: 2356: 2351: 2350: 2349: 2342:Bioprospecting 2339: 2333: 2331: 2325: 2324: 2322: 2321: 2320: 2319: 2314: 2304: 2303: 2302: 2297: 2292: 2287: 2277: 2276: 2275: 2270: 2269: 2268: 2263: 2253: 2252: 2251: 2246: 2236: 2235: 2234: 2224: 2219: 2209: 2208: 2207: 2197: 2196: 2195: 2185: 2184: 2183: 2178: 2173: 2168: 2158: 2153: 2148: 2147: 2146: 2145: 2144: 2128: 2126: 2120: 2119: 2117: 2116: 2111: 2110: 2109: 2104: 2094: 2089: 2084: 2079: 2057: 2052: 2047: 2041: 2039: 2033: 2032: 2029: 2028: 2026: 2025: 2020: 2015: 2009: 2007: 2003: 2002: 2000: 1999: 1994: 1993: 1992: 1987:Clean Air Act 1979: 1974: 1969: 1960: 1958: 1949: 1943: 1942: 1937: 1935: 1934: 1927: 1920: 1912: 1903: 1902: 1900: 1899: 1893: 1891: 1890:Related topics 1887: 1886: 1884: 1883: 1877: 1872: 1867: 1862: 1856: 1854: 1850: 1849: 1847: 1846: 1841: 1836: 1830: 1828: 1824: 1823: 1821: 1820: 1815: 1810: 1805: 1800: 1794: 1792: 1786: 1785: 1783: 1782: 1777: 1772: 1767: 1761: 1759: 1753: 1752: 1750: 1749: 1744: 1739: 1734: 1729: 1724: 1719: 1713: 1711: 1705: 1704: 1702: 1701: 1696: 1691: 1686: 1681: 1676: 1670: 1668: 1662: 1661: 1658: 1656: 1655: 1648: 1641: 1633: 1622: 1621: 1594: 1573: 1555: 1548: 1506: 1499: 1460: 1435: 1424:(2): 181–195. 1408: 1353: 1318:(3): 835–965. 1298: 1271:(1): 225–262. 1251: 1200: 1178: 1128: 1113: 1088: 1081: 1055: 1028:(5): 605–620. 1012: 1003: 981: 951: 873: 847: 826: 825: 823: 820: 819: 818: 813: 808: 802: 797: 792: 787: 782: 777: 772: 767: 762: 757: 752: 747: 742: 736: 735: 719: 716: 715: 714: 709: 704: 699: 692: 689: 680:flash flooding 666: 663: 629:water scarcity 617: 609: 601: 600:Climate change 598: 596: 593: 548: 545: 528: 525: 507: 504: 471: 468: 391:field capacity 386: 383: 367:biodegradation 325: 322: 296: 293: 247:surface runoff 218: 215: 209: 206: 204: 201: 128: 127: 42: 40: 33: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 3636: 3625: 3622: 3620: 3617: 3615: 3612: 3610: 3607: 3605: 3602: 3600: 3597: 3595: 3592: 3590: 3587: 3585: 3582: 3580: 3577: 3575: 3572: 3570: 3567: 3565: 3562: 3560: 3557: 3556: 3554: 3539: 3530: 3529: 3526: 3520: 3517: 3515: 3512: 3510: 3507: 3505: 3502: 3500: 3497: 3495: 3492: 3490: 3487: 3485: 3482: 3480: 3477: 3475: 3472: 3470: 3467: 3465: 3462: 3460: 3457: 3455: 3452: 3450: 3447: 3446: 3444: 3440: 3434: 3431: 3429: 3426: 3424: 3421: 3419: 3416: 3414: 3411: 3409: 3406: 3404: 3401: 3399: 3396: 3394: 3391: 3389: 3386: 3384: 3381: 3379: 3378:Sedimentation 3376: 3374: 3371: 3369: 3366: 3364: 3361: 3359: 3356: 3354: 3351: 3349: 3346: 3344: 3341: 3339: 3336: 3334: 3331: 3329: 3326: 3324: 3321: 3319: 3316: 3314: 3311: 3309: 3306: 3304: 3301: 3299: 3296: 3294: 3291: 3289: 3286: 3284: 3281: 3279: 3276: 3275: 3273: 3271: 3267: 3261: 3258: 3256: 3253: 3251: 3248: 3246: 3243: 3241: 3238: 3236: 3233: 3231: 3228: 3226: 3223: 3221: 3218: 3216: 3213: 3211: 3208: 3206: 3203: 3201: 3198: 3197: 3195: 3193: 3189: 3183: 3180: 3178: 3175: 3173: 3172:Sewage sludge 3170: 3168: 3165: 3163: 3160: 3158: 3155: 3153: 3150: 3148: 3145: 3143: 3140: 3138: 3135: 3133: 3130: 3128: 3125: 3123: 3120: 3118: 3115: 3113: 3110: 3108: 3105: 3103: 3100: 3098: 3097:Cooling water 3095: 3093: 3092:Cooling tower 3090: 3088: 3085: 3083: 3080: 3078: 3075: 3073: 3070: 3068: 3065: 3063: 3060: 3058: 3057:Ballast water 3055: 3053: 3050: 3049: 3047: 3043: 3039: 3032: 3027: 3025: 3020: 3018: 3013: 3012: 3009: 2997: 2989: 2988: 2985: 2975: 2974:Non-renewable 2971: 2968: 2966: 2963: 2961: 2958: 2956: 2953: 2951: 2948: 2946: 2940: 2938: 2935: 2934: 2932: 2930: 2926: 2920: 2917: 2915: 2914:Urban ecology 2912: 2910: 2907: 2903: 2900: 2899: 2898: 2895: 2893: 2890: 2886: 2883: 2881: 2878: 2877: 2876: 2873: 2869: 2866: 2865: 2864: 2861: 2857: 2854: 2852: 2849: 2848: 2847: 2844: 2842: 2839: 2835: 2832: 2830: 2827: 2826: 2825: 2822: 2818: 2815: 2813: 2810: 2808: 2805: 2803: 2800: 2799: 2798: 2795: 2794: 2791: 2788: 2784: 2772: 2769: 2767: 2764: 2763: 2762: 2759: 2757: 2754: 2752: 2749: 2747: 2746:Privatization 2744: 2742: 2739: 2737: 2734: 2732: 2729: 2727: 2724: 2722: 2719: 2717: 2714: 2712: 2709: 2707: 2704: 2700: 2697: 2696: 2695: 2692: 2690: 2687: 2685: 2682: 2680: 2677: 2675: 2672: 2671: 2669: 2665: 2659: 2656: 2652: 2649: 2648: 2647: 2644: 2642: 2641:Surface water 2639: 2637: 2634: 2630: 2627: 2626: 2625: 2622: 2620: 2617: 2613: 2612: 2608: 2607: 2606: 2603: 2599: 2596: 2594: 2591: 2589: 2586: 2585: 2584: 2581: 2579: 2576: 2572: 2569: 2567: 2564: 2562: 2559: 2558: 2557: 2554: 2552: 2549: 2547: 2544: 2540: 2537: 2536: 2535: 2532: 2531: 2529: 2525: 2522: 2520: 2516: 2508: 2505: 2503: 2500: 2499: 2498: 2495: 2493: 2490: 2488: 2485: 2481: 2478: 2476: 2473: 2471: 2468: 2466: 2463: 2461: 2458: 2456: 2453: 2451: 2448: 2447: 2446: 2443: 2441: 2438: 2436: 2433: 2431: 2428: 2424: 2421: 2420: 2419: 2416: 2412: 2409: 2407: 2404: 2402: 2399: 2397: 2394: 2393: 2392: 2389: 2385: 2382: 2380: 2377: 2375: 2372: 2371: 2370: 2367: 2365: 2362: 2360: 2357: 2355: 2352: 2348: 2345: 2344: 2343: 2340: 2338: 2335: 2334: 2332: 2330: 2326: 2318: 2315: 2313: 2310: 2309: 2308: 2305: 2301: 2298: 2296: 2293: 2291: 2288: 2286: 2283: 2282: 2281: 2278: 2274: 2271: 2267: 2264: 2262: 2259: 2258: 2257: 2254: 2250: 2247: 2245: 2242: 2241: 2240: 2237: 2233: 2230: 2229: 2228: 2225: 2223: 2220: 2218: 2215: 2214: 2213: 2210: 2206: 2203: 2202: 2201: 2198: 2194: 2191: 2190: 2189: 2186: 2182: 2179: 2177: 2174: 2172: 2169: 2167: 2164: 2163: 2162: 2159: 2157: 2154: 2152: 2149: 2143: 2142:peak farmland 2140: 2139: 2138: 2135: 2134: 2133: 2130: 2129: 2127: 2125: 2121: 2115: 2112: 2108: 2105: 2103: 2100: 2099: 2098: 2095: 2093: 2090: 2088: 2085: 2083: 2080: 2077: 2073: 2069: 2065: 2061: 2058: 2056: 2053: 2051: 2048: 2046: 2043: 2042: 2040: 2038: 2034: 2024: 2021: 2019: 2016: 2014: 2011: 2010: 2008: 2004: 1998: 1995: 1991: 1985: 1984: 1983: 1980: 1978: 1975: 1973: 1970: 1968: 1962: 1961: 1959: 1957: 1953: 1950: 1948: 1944: 1940: 1933: 1928: 1926: 1921: 1919: 1914: 1913: 1910: 1898: 1895: 1894: 1892: 1888: 1881: 1878: 1876: 1873: 1871: 1868: 1866: 1863: 1861: 1858: 1857: 1855: 1851: 1845: 1842: 1840: 1837: 1835: 1832: 1831: 1829: 1827:Problem soils 1825: 1819: 1816: 1814: 1811: 1809: 1806: 1804: 1801: 1799: 1796: 1795: 1793: 1791: 1787: 1781: 1778: 1776: 1773: 1771: 1768: 1766: 1763: 1762: 1760: 1758: 1754: 1748: 1745: 1743: 1740: 1738: 1735: 1733: 1730: 1728: 1725: 1723: 1722:Tile drainage 1720: 1718: 1715: 1714: 1712: 1710: 1706: 1700: 1697: 1695: 1692: 1690: 1687: 1685: 1682: 1680: 1677: 1675: 1672: 1671: 1669: 1667: 1663: 1654: 1649: 1647: 1642: 1640: 1635: 1634: 1631: 1627: 1611: 1610:pubs.usgs.gov 1607: 1601: 1599: 1595: 1590: 1586: 1580: 1578: 1574: 1566: 1559: 1556: 1551: 1545: 1541: 1537: 1533: 1532: 1524: 1517: 1515: 1513: 1511: 1507: 1502: 1496: 1492: 1488: 1484: 1483: 1475: 1467: 1465: 1461: 1458: 1453: 1448: 1442: 1440: 1436: 1431: 1427: 1423: 1419: 1412: 1409: 1404: 1400: 1396: 1392: 1388: 1384: 1380: 1376: 1372: 1368: 1364: 1357: 1354: 1349: 1345: 1341: 1337: 1333: 1329: 1325: 1321: 1317: 1313: 1309: 1302: 1299: 1294: 1290: 1286: 1282: 1278: 1274: 1270: 1266: 1262: 1255: 1252: 1247: 1243: 1239: 1235: 1231: 1227: 1223: 1219: 1215: 1211: 1204: 1201: 1198: 1193: 1188: 1182: 1179: 1174: 1170: 1166: 1162: 1158: 1154: 1150: 1146: 1139: 1132: 1129: 1124: 1120: 1116: 1110: 1106: 1105: 1097: 1095: 1093: 1089: 1084: 1078: 1074: 1070: 1066: 1059: 1056: 1051: 1047: 1043: 1039: 1035: 1031: 1027: 1023: 1016: 1013: 1007: 1004: 991: 985: 982: 969: 965: 961: 955: 952: 949: 944: 938: 934: 930: 926: 921: 916: 912: 908: 905:(3): 034012. 904: 900: 896: 888: 886: 884: 882: 880: 878: 874: 871: 867: 864: 858: 854: 850: 844: 840: 839: 831: 828: 821: 817: 814: 812: 809: 806: 803: 801: 798: 796: 793: 791: 788: 786: 783: 781: 778: 776: 773: 771: 768: 766: 763: 761: 758: 756: 753: 751: 748: 746: 743: 741: 738: 737: 733: 727: 722: 717: 713: 710: 708: 705: 703: 700: 698: 695: 694: 690: 688: 685: 681: 676: 672: 664: 659: 655: 651: 648: 644: 641: 636: 634: 630: 626: 622: 614: 607: 599: 594: 592: 590: 586: 582: 578: 574: 570: 566: 562: 558: 555:, using such 554: 546: 544: 542: 538: 534: 526: 524: 521: 517: 513: 505: 503: 501: 496: 492: 489: 485: 481: 480:transpiration 477: 469: 467: 465: 461: 457: 453: 449: 444: 442: 438: 434: 430: 426: 422: 418: 414: 409: 407: 402: 400: 396: 392: 384: 382: 380: 376: 372: 368: 364: 360: 355: 353: 338: 334: 329: 323: 321: 319: 314: 313:mineral soils 310: 306: 301: 294: 292: 290: 287: 283: 279: 275: 271: 266: 264: 260: 256: 252: 248: 244: 240: 236: 232: 223: 216: 214: 207: 202: 200: 196: 194: 190: 186: 182: 178: 174: 170: 166: 162: 161:surface water 158: 154: 150: 146: 145:deep drainage 142: 136:Water balance 134: 124: 121: 113: 110:November 2008 102: 99: 95: 92: 88: 85: 81: 78: 74: 71: â€“  70: 66: 65:Find sources: 59: 55: 49: 48: 43:This article 41: 37: 32: 31: 19: 3589:Soil physics 3584:Liquid water 3519:Vacuum sewer 3458: 3403:Sewer mining 3353:Ion exchange 3303:Chlorination 3225:Heavy metals 3182:Urban runoff 3122:Ion exchange 3102:Fecal sludge 2972: / 2846:Exploitation 2731:Conservation 2674:Desalination 2609: 2565: 2502:conservation 2337:Biodiversity 2285:conservation 2132:Agricultural 2060:Fossil fuels 1844:Saline soils 1839:Alkali soils 1625: 1613:. 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Retrieved 968:the original 963: 954: 902: 898: 837: 830: 732:Water portal 674: 671:urbanization 668: 665:Urbanization 657: 653: 645: 637: 618: 550: 530: 519: 515: 512:soil physics 509: 497: 493: 488:infiltration 473: 445: 410: 406:arid regions 403: 398: 388: 379:rain gardens 361:collects in 356: 333:over-pumping 330: 327: 298: 267: 228: 211: 197: 175:below plant 148: 144: 140: 139: 116: 107: 97: 90: 83: 76: 64: 52:Please help 47:verification 44: 3509:Storm drain 3504:Sewage farm 3428:Vermifilter 3383:Septic tank 3343:Imhoff tank 3240:Temperature 3147:Return flow 3137:Papermaking 2965:Nationalism 2937:Common-pool 2578:Hydrosphere 2571:remediation 2556:Groundwater 2151:Degradation 1790:Groundwater 996:October 31, 974:October 31, 838:Groundwater 640:water cycle 589:vadose zone 476:evaporation 460:groundwater 456:water table 413:contaminant 395:groundwater 344:1,800 crore 274:groundwater 255:sustainable 189:water cycle 185:water table 173:vadose zone 165:groundwater 3553:Categories 3474:Irrigation 3338:Filtration 3038:Wastewater 2960:Extraction 2919:Wilderness 2880:accounting 2863:Management 2829:ecological 2817:tragedy of 2736:Peak water 2721:Efficiency 2694:Sanitation 2636:Stormwater 2629:harvesting 2605:Irrigation 2507:management 2465:gene banks 2406:management 2384:management 2300:resilience 2266:phosphorus 2222:industrial 2200:Management 2176:soundscape 2082:Geothermal 1818:Watertable 1666:Irrigation 1615:2019-03-22 1523:"4. 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Aquifer recharge

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hydrologic
water
surface water
groundwater
aquifer
vadose zone
roots
flux
water table
water cycle
reclaimed water

rain
snow
logging
topsoil
surface runoff

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