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Unit 4 Running Water and Ground Water SED201

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Unit 4- Running Water and Ground
Water
Source:
https://www.google.com/url?sa=i&url=https%3A%2F%2Fwww.the71percent.org%2Findustrialwaterusage%2F&psig=AOvVaw0t4gOAlFYZdq4smY_E_Aam&ust=1644161658079000&source=images&cd=vfe&ved=0CAsQjRxqFwoTCICadPx6PUCFQAAAAAdAAAAABAR
WATER WITHDRAWAL
Municipalities (households,
services)
16%
Industries
12%
Agriculture
72%
Source: https://www.unwater.org/water-facts/scarcity/
Nearly half the global population are already living in
potential water scarce areas at least one month per year
and this could increase to some 4.8–5.7 billion in 2050.
About 73% of the affected people live in Asia (69% by
2050). (Burek et al., 2016)
Source: https://www.unwater.org/water-facts/scarcity/
In the Philippines, around 1 in 10 people still do not
have access to improved water sources.
Source:
https://www.who.int/philippines/news/feature-stories/detail/water-shortage-in-the-philippines-threatenssustainable-development-and-health
The Manila Water Company Inc. and Manila Water
Philippine Venture Inc. signed an P8-billion concession
agreement with the provincial government to supply the
province with potable water.
Source: https://tribune.net.ph/index.php/2022/01/17/pangasinan-water-supply-sees-boost/
THE WATER
CYCLE
Of the many processes
involved in the water
cycle, the most
important
are evaporation,
transpiration,
condensation,
precipitation, and
runoff.
Source: https://gwconsortium.org/public-education/what-is-the-water-cycle/
Running Water
• Runoff, gravity-driven flow across
Earth’s surface, depends on
infiltration capacity of the surface
material.
Source: https://www.lakeheadu.ca/sites/default/files/uploads/54/Geology%203015%20Week%209b.pdf
River
Source: https://www.google.com/url?sa=i&url=https%3A%2F%2Friverbasin.denr.gov.ph%2Friver%2Fagno&psig=AOvVaw3R2ODMduiufDFH016V n8z&ust=1644169047855000&source=images&cd=vfe&ved=0CAsQjRxqFwoTCPCxkpaN6fUCFQAAAAAdAAAAABAs
Streams
Source: https://www.nationalgeographic.org/article/streams/
PROCESSES INVOLVED
.
• Sheet flow occurs when a more-or-less continuous
sheet of shallow water moves over the surface.
• Channel flow is confined to long, trough-like
depressions ranging in size from tiny rills to huge rivers.
Source: https://qsstudy.com/wp-content/uploads/2017/11/Overland-flow-of-Running-Water.jpg
Within a
stream
channel,
three types
flow can be
observed:
Source: https://blog.exair.com/wp-content/uploads/2018/03/ky-spill-way.png
EROSION AND TRANSPORT
Running water is an agent of erosion
• Streams move material in a variety of ways
• Bed load
• Suspended load
• Saltation
• Dissolved load
DEPOSITION BY RUNNING WATER
• Sediment can be transported great distances by rivers,
but it is eventually deposited.
• Deposition may take place within the channel, on the
floodplain, at the mouth of the river where it enters a lake
or the sea, or where the river flows from the mountains on
to a flat valley floor.
GROUNDWATER
• Groundwater is water that exists underground in saturated
zones beneath the land surface.
• Groundwater is the part of precipitation that seeps down
through the soil until it reaches rock material that is saturated
with water. Water in the ground is stored in the spaces between
rock particles
Source: https://www.usgs.gov/faqs/what-groundwater
Source: https://www.watereducation.org/sites/main/files/imagecache/medium/main-images/USGS-GW.png?1637047272
Source: https://ppdo.pangasinan.gov.ph/provincial-map/ground-water-map/
NATURAL AND ARTIFICIAL RECHARGE OF
GROUNDWATER
• Natural refilling of deep aquifers is a slow process because
groundwater moves slowly through the unsaturated zone and the
aquifer (Infiltration)
• Aquifers may be artificially recharged in two main ways:
*Rapid-infiltration pits: One way is to spread water over the
land in pits, furrows, or ditches, or to erect small dams in stream
channels to detain and deflect surface runoff, thereby allowing it to
infiltrate to the aquifer
*Groundwater injection: The other way is to construct
recharge wells and inject water directly into an aquifer
Source: https://www.usgs.gov/special-topics/water-science-school/science/infiltration-and-water-cycle
According to the World Health Organization, 1 in 10
people in the Philippines still do not have access to
improved water sources, but the government is working
to achieve universal coverage for water by 2028.
Source: https://www.who.int/philippines/news/feature-stories/detail/water-shortage-in-the-philippines-threatens-sustainable-development-and-health
Based on an Annual Poverty
Indicators
Survey,
94
percent of Filipino families
have access to improved
water sources, and around
77 percent of these families
do not implement additional
water treatment processes
to guarantee the safety of
their water sources.
Source: https://www.wateroam.com/socialawareness/the-water-crisis-philippines
The World Health Organization is working with the Philippines Department of
Health and other sector agencies to ensure safe water for all through the
development and implementation of water safety planning, strengthening
systems and capacity for drinking-water quality surveillance and monitoring,
and improvement of water, sanitation, and hygiene in health care facilities.
Source: https://www.who.int/philippines/news/feature-stories/detail/water-shortage-in-the-philippines-threatens-sustainable-development-and-health
THREAT
Water Quality
• Pollution of groundwater may come from domestic
wastewater, agricultural runoffs, and industrial effluents. This
occurs when contaminants reach the aquifer or water table in
the form of leachate.
Source: Philippine Environnent Monitor 2003
http://www.wepadb.net/policies/state/philippines/groundwater.htm#:~:text=Groundwater%20is%20replenished%20or%20recharged,resource%20potential%20of%20the%20Philippines.&text=Groundwater%20is%20used%20for%20drinking,the%20people%20in%20the%20
country.
DIFFERENCE BETWEEN RUNNING WATER AND
GROUND WATER
In Terms of:
Ground Water
Location Beneath the surface of the
earth
Running Water
On the surface of the earth
Pollution less prone
highly prone
Occurrence groundwater table, aquifers,
soil pore spaces
Uses household needs, agricultural
needs, and industrial purposes
Rivers, streams/brooks
drinking, cleaning, irrigation
purposes, agricultural needs,
wastewater treatment,
livestock, hydropower
production, etc.
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