<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="sk">
	<id>https://geonika.agis.uniba.sk/tsenz/index.php?action=history&amp;feed=atom&amp;title=Groundwater_recharge</id>
	<title>Groundwater recharge - História úprav</title>
	<link rel="self" type="application/atom+xml" href="https://geonika.agis.uniba.sk/tsenz/index.php?action=history&amp;feed=atom&amp;title=Groundwater_recharge"/>
	<link rel="alternate" type="text/html" href="https://geonika.agis.uniba.sk/tsenz/index.php?title=Groundwater_recharge&amp;action=history"/>
	<updated>2026-04-06T08:22:11Z</updated>
	<subtitle>História úprav pre túto stránku na wiki</subtitle>
	<generator>MediaWiki 1.31.1</generator>
	<entry>
		<id>https://geonika.agis.uniba.sk/tsenz/index.php?title=Groundwater_recharge&amp;diff=270&amp;oldid=prev</id>
		<title>Vrut: Importing text file</title>
		<link rel="alternate" type="text/html" href="https://geonika.agis.uniba.sk/tsenz/index.php?title=Groundwater_recharge&amp;diff=270&amp;oldid=prev"/>
		<updated>2014-08-05T14:54:25Z</updated>

		<summary type="html">&lt;p&gt;Importing text file&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Nová stránka&lt;/b&gt;&lt;/p&gt;&lt;div&gt;:Slovak term: [[Slovenský termín]]&lt;br /&gt;
# Groundwater recharge should be defined as the downward flow of water reaching the water table and replenishing groundwater resources (WHO 2006).&lt;br /&gt;
&lt;br /&gt;
==Explanation==&lt;br /&gt;
It is important to distinguish between infiltration of precipitation and groundwater&lt;br /&gt;
recharge. When rain falls, some infiltrates into the soil. Much of this moisture is taken up&lt;br /&gt;
by the roots of plants and is subject to evapotranspiration from the soil zone, and some&lt;br /&gt;
becomes interflow drainage to streams and rivers. Only a part of the infiltration becomes&lt;br /&gt;
recharge and moves deeper into the subsurface under gravity, and in arid and semi-arid&lt;br /&gt;
areas this may be a very small proportion indeed (WHO 2006).&lt;br /&gt;
&lt;br /&gt;
==Example==&lt;br /&gt;
Now that the hydrological cycle has been interfered with as a result of human activities,&lt;br /&gt;
recharge can also be derived from canals, reservoirs, irrigated land, water mains and&lt;br /&gt;
sewerage systems in urban areas, mining waste, sewage lagoons -in fact - any artificial&lt;br /&gt;
water body that is in connection with the subsurface. Artificial recharge, which is becoming&lt;br /&gt;
an increasingly important resource management option, can also introduce water of&lt;br /&gt;
different origin and quality into aquifers. This of course means that groundwater recharge&lt;br /&gt;
is not always of the same good quality as infiltrating rainfall, which itself may be&lt;br /&gt;
contaminated by acid rain or atmospheric acid deposition (WHO 2006).&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
* WHO (2006) [http://www.who.int/water_sanitation_health/publications/protecting_groundwater/en/index.html Protecting groundwater for health.]&lt;br /&gt;
&lt;br /&gt;
==Links==&lt;br /&gt;
* [http://apps.who.int/thelexicon/ WHO — The Health and Environment Lexicon]&lt;br /&gt;
&lt;br /&gt;
[[Category:EN]]&lt;/div&gt;</summary>
		<author><name>Vrut</name></author>
		
	</entry>
</feed>