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3.2. Practise reading of the following words and word-combinations from the text.

To saturate, saturated, unsaturated;

Pore, porous;

Exist, existence, existing;

Stone, limestone, sandstone;

To accumulate, accumulated, accumulation;

A result, resulting, to result in;

To dissolve, dissolution, dissolvent, to be dissolved by;

Wet, to wet, wetness;

To support, a support, supporter;

Dense, density;

To serve, server, service;

To supply, supply.

3.3. Read aloud and give Ukrainian equivalents of the following international words:

ocean, diagram, vegetation, zone, pore, practical, safe, nature, industrialized, municipal, installation, community, bacteria, pathogenic, economical, distributor, stratum, natural, mineral, pump, gravity, factor, surprise, center, solid, granite, type, to accumulate, result, vertical.

3.4. Memorize the spelling, pronunciation and translation of the following words:

precipitation

опади

to seep

просочуватися

rock material

скеляста порода

to saturate

насичувати

water table

рівень ґрунтових вод

to support

підтримувати

to fill

наповнювати

to penetrate

проникати

clay

глина

particle

часточка

crack

щілина, тріщина

fracture

розлом, розрив

bedrock

корінна, материнська порода (геол.)

dense

щільний

sandstone

піщаник

limestone

вапняк

to dissolve

розчиняти

cavity

порожнина, пустота, щілина в породі

to lay in layers

залягати шарами

to pool

розливатися

aquifer

водоносний горизонт

3.5. Read the text “Earth’s Water: Ground Water” and do the following:

1. Define

• what the text deals with:

• quality of ground water and factors determining it;

• various types of rocks and availability of ground water in then;

• the location of ground water in the Earth’s crust and factors responsible for its existence.

2. Translate the text into Ukrainian.

Text a. Earth's water: ground water

1. Ground water is the part of precipitation that seeps down through the soil until it reaches rock material that is saturated with water. Ground water slowly moves underground, generally at a downward angle (because of gravity), and may eventually seep into streams, lakes, and oceans.

unsaturated soil

unsaturated soil

2. Here is a simplified diagram showing how the ground is saturated below the water table. The ground above the water table may be wet to a certain degree, but it does not stay saturated. The dirt and rock in this unsaturated zone contain air and some water and support the vegetation on the Earth. The saturated zone below the water table has water that fills the tiny spaces (pores) between rock particles and the cracks (fractures) of the rocks.

3. A few important factors are responsible for the existence of ground water:

(a) Gravity

Nothing surprising here – gravity pulls water toward the center of the Earth. That means that water on the surface will try to seep into the ground below it.

(b) The Rocks Below Our Feet

The rock below the Earth's surface is the bedrock. If all bedrock consisted of a dense material like solid granite, then even gravity would have a hard time pulling water downward. But Earth's bedrock consists of many types of rock, such as sandstone, granite, and limestone. Bedrocks have varying amounts of void spaces in them where ground water accumulates. Bedrock can also become broken and fractured creating spaces that can fill with water. And some bedrock, such as limestone, are dissolved by water – which results in large cavities that fill with water.

4. In many places, you can see that rock is laid down in layers. Some layers have rocks that are more porous than others, and here water moves more freely (in a horizontal manner) through the earth.

5. So, gravity doesn't pull water all the way to the center of the Earth. Deep in the bedrock there are rock layers made of dense material, such as granite, or material that water has a hard time penetrating, such as clay. These layers are under the porous rock layers. Since it is more difficult for the water to go any deeper, it tends to pool in the porous layers and flow in a more horizontal direction across the aquifer toward a surface-water body, like a river.

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