Chapter 6 : Hydrology and Soil
Hydrological
Cycle (Water Cycle)
When
water evaporates from land or sea, it enters the atmosphere as vapor. When the
moisture in the atmosphere cools, it condenses into cloud. Finally, it becomes
rain or snow and falls down to the earth¡¦s surface again. Part of it seeps
underground and becomes groundwater; the rest of it trickles down into rivers
and lakes and flows into the ocean. The earth¡¦s water is continuously cycled
from the atmosphere to the earth, from the earth to the ocean, and from the
ocean back to the atmosphere. This cycle is called the ¡§Hydrological Cycle.¡¨
When
rain falls, it follows the terrain of the earth and forms small rivulets. These
rivulets combine to form tiny creeks. As more and more tiny creeks merge, they
gradually form rivers. If we look down from the sky or check a map, we will
find that rivers often have many tributaries. Together, the main stream and its
tributaries make up a river system. River systems are divided by watersheds,
which are usually mountain ranges. Each river system has a drainage area; the
precipitation that falls within this area either evaporates or flows into the river.
So we can also say that watersheds separate drainage areas.
River
Systems in Taiwan
Figure
6-1 shows the distributions of rivers in Taiwan. There are 129 rivers of
different sizes. The river density of Taiwan is very high. The rivers are
distributed throughout the island, so that if you look at a map of Taiwan¡¦s rivers, you basically see an outline of
Taiwan.
Taiwan
is a long and narrow mountainous island, so its rivers are relatively short. There
are only six rivers longer than 100 kilometers. Taiwan¡¦s
shape and terrain result in riverbeds with very steep gradients. In other
words, Taiwan¡¦s
rivers flow downhill very quickly and there are a lot of rapids. They also have
considerable washout power. Seasonal rainfall variations result in tremendous
differences in river volume. During summer, torrential rains cause rivers to
swell and surge furiously. Such a river is a spectacular sight but also very dangerous.
Winter is the dry season. The rivers in southern Taiwan shrink to tiny creeks, or
dry up leaving nothing but dust and gravel.
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Figure 6-1 The River Systems of Taiwan
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River
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River
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River (Wu
River)
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River
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River
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River
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Water
Resources
The
average annual rainfall of Taiwan
is around 2,500 mm,
almost 3.5 times of the average global rainfall. If we subtract evaporation
from precipitation, the remainder is the water we can tap as a resource.
Although the rainfall of Taiwan
is abundant, the population density is also high. In addition, terrain and
weather reduce the amount water that is actually available. The result is that Taiwan
has a water problem: per capita Taiwanese people are relatively water deprived.
Taiwan¡¦s
per capita water supply is only half the world average. Water conservancy
facilities such as reservoirs, ponds and pools are used to store water and
maintain the water supply.
Taiwan¡¦s
water resources include surface and groundwater. Water is consumed by households,
traditional farms for irrigation, fish farms, and industry.
In
recent years, improper land use and outright exploitation have polluted Taiwan¡¦s
water. In some areas, excessive pumping of groundwater has caused serious
environmental problems like stratum subsidence. There is an urgent need for
effective governmental regulation.
Soil
The
rocks on the surface of the earth will become soil after long-term weathering.
They will form different kinds of soil depending on terrain, climate, time, and
what organisms live in the soil. Different soils vary in color, viscosity, and
particle size. These features determine what we can do with a certain kind of
soil. The three main soil types of in Taiwan include laterite and loess,
both of which are formed by weathering, and alluvial soil, which is deposited
by rivers. Human beings put different kinds of soil to different uses. When
deciding land usage, we also take terrain into account.
The
formation of soil is a slow process. Even a thin layer of soil takes at least
three to five hundred years to form. With some types of soil in certain
conditions, a thin layer may even take thousands of years to form. However, it
does not take long for it to wash away in a torrential rain. When willful human
exploitation is unrestrained by effective water and soil conservation policy,
washout erosion becomes a serious problem. Once washed away, soil can never be
reclaimed.
Soil
is also susceptible to pollution. The main sources of pollution are homes and
factories that discharge enormous amounts of untreated waste water contaminated
with heavy metals. Farmers who use excessive pesticides and fertilizers add to
the pollution problem. These noxious substances contaminate the soil, threatening
people¡¦s health through bioaccumulation. Therefore, protecting the soil from
erosion and pollution is important for everyone.
Water
and Soil Conservation and Wildlife
Taiwan
is a beautiful, densely-wooded island. The ecological environment allows
wildlife to thrive. Many species of wild animals once inhabited the entire length
of the island. Place names such as Lugang, literally
Deer Harbor,
give us an indication of the richness of animal life in the past. As the human population
of Taiwan
grew, habitat for wildlife was reduced. The number of wild animals and even
plants declined. This is still happening today: many species of the wildlife
are endangered or already extinct. Deforestation makes it even harder to
maintain water and soil balance.
Plants
need to assimilate nutrients and water from the soil in order to grow. Plants also
protect the soil from washout. Taiwan¡¦s
abundant rainfall and steep terrain mean that washout is still a serious
problem. Without proper water and soil conservation, the ecological environment
may suffer irrevocable damage. Instead of merely seeking short-term benefits, we
should put more effort into water and soil conservation, especially on
slopeland. This is the only way to ensure a sustainable ecological environment.