Hydrology assignment. Description and meanings., Assignments of Hydrology

What is hydrology. What are its branches.

Typology: Assignments

2020/2021

Uploaded on 02/03/2021

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Finals: Assignment # 1
Due: November 19, 2020
1. Identify and define/explain at least 20 important terms that you can find in Lesson # 1.
๏ƒ˜ The unsaturated zone or vadose zone extends above the water table and includes the
soil water zone down to the water table, which divides the unsaturated zone from the
saturated zone.
๏ƒ˜ The water table is defined as the level to which water will rise in a well drilled into the
saturated zone.
๏ƒ˜ The soil water zone, which extends from the ground surface down through the major
root zone, varies with soil type and vegetation. The amount of water present in the soil
water zone depends primarily on recent exposure to rainfall and infiltration.
๏ƒ˜ Hygroscopic water remains adsorbed to the surface of soil grains.
๏ƒ˜ Gravitational water drains through the soil under the influence of gravity.
๏ƒ˜ Capillary water is held in the zone just above the water table and exists because water
can be pulled upward from the water table by surface tension.
๏ƒ˜ The capillary zone, or fringe, extends from the water table up to the limit of capillary
rise, which varies inversely with the pore size of the soil and directly with the surface
tension.
๏ƒ˜ Capillary rise can range from a few cm for fine gravel to more than 200 cm for silt
(Todd and Mays, 2005).
๏ƒ˜ In the saturated zone, which occurs beneath the water table, the porosity is a direct
measure of the water contained per unit volume, expressed as the ratio of the volume of
voids to the total volume.
๏ƒ˜ Specific yield is defined as the volume of water released from an unconfined aquifer per
unit surface area per unit head decline in the water table.
๏ƒ˜ A well is a vertical hole dug into the earth, usually cased with metal or PVC plastic up to
the land surface.
๏ƒ˜ The portion of the well hole that is open to the aquifer is screened to prevent aquifer
material from entering the well.
๏ƒ˜ A vertical penetration used to collect soil or water samples that is not cased is called a
borehole.
๏ƒ˜ An aquifer can be defined as a formation that contains sufficient permeable material to
yield significant quantities of water to wells and springs. Aquifers are generally areally
extensive and may be overlain or underlain by confining beds. Most aquifers can be
considered underground storage reservoirs that receive recharge from rainfall or from an
artificial source. Water flows out of an aquifer due to gravity or to pumping from wells.
๏ƒ˜ An aquiclude is saturated and is a relatively impermeable confining unit, such as clay,
that might act as a confining layer above or below an aquifer system.
๏ƒ˜ An aquitard is a saturated, low permeability stratum, such as a silty clay, that may leak
water from one aquifer to another.
๏ƒ˜ Aquifers may be classified as unconfined, depending on the existence of a water table,
defined by levels in shallow wells.
๏ƒ˜ A confined aquifer is one that is overlain by a confining unit and is under pressure.
๏ƒ˜ A leaky confined aquifer represents a stratum that allows water to flow from above
through the confining zone.
๏ƒ˜ A perched water table is an example where an unconfined water body sits on top of a
clay lens, separated from the main aquifer below.
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Finals: Assignment # 1 Due: November 19, 2020

1. Identify and define/explain at least 20 important terms that you can find in Lesson # 1.

๏ƒ˜ The unsaturated zone or vadose zone extends above the water table and includes the soil water zone down to the water table, which divides the unsaturated zone from the saturated zone. ๏ƒ˜ The water table is defined as the level to which water will rise in a well drilled into the saturated zone. ๏ƒ˜ The soil water zone , which extends from the ground surface down through the major root zone, varies with soil type and vegetation. The amount of water present in the soil water zone depends primarily on recent exposure to rainfall and infiltration. ๏ƒ˜ Hygroscopic water remains adsorbed to the surface of soil grains. ๏ƒ˜ Gravitational water drains through the soil under the influence of gravity. ๏ƒ˜ Capillary water is held in the zone just above the water table and exists because water can be pulled upward from the water table by surface tension. ๏ƒ˜ The capillary zone , or fringe, extends from the water table up to the limit of capillary rise, which varies inversely with the pore size of the soil and directly with the surface tension. ๏ƒ˜ Capillary rise can range from a few cm for fine gravel to more than 200 cm for silt (Todd and Mays, 2005). ๏ƒ˜ In the saturated zone, which occurs beneath the water table, the porosity is a direct measure of the water contained per unit volume, expressed as the ratio of the volume of voids to the total volume. ๏ƒ˜ Specific yield is defined as the volume of water released from an unconfined aquifer per unit surface area per unit head decline in the water table. ๏ƒ˜ A well is a vertical hole dug into the earth, usually cased with metal or PVC plastic up to the land surface. ๏ƒ˜ The portion of the well hole that is open to the aquifer is screened to prevent aquifer material from entering the well. ๏ƒ˜ A vertical penetration used to collect soil or water samples that is not cased is called a borehole. ๏ƒ˜ An aquifer can be defined as a formation that contains sufficient permeable material to yield significant quantities of water to wells and springs. Aquifers are generally areally extensive and may be overlain or underlain by confining beds. Most aquifers can be considered underground storage reservoirs that receive recharge from rainfall or from an artificial source. Water flows out of an aquifer due to gravity or to pumping from wells. ๏ƒ˜ An aquiclude is saturated and is a relatively impermeable confining unit, such as clay, that might act as a confining layer above or below an aquifer system. ๏ƒ˜ An aquitard is a saturated, low permeability stratum, such as a silty clay, that may leak water from one aquifer to another. ๏ƒ˜ Aquifers may be classified as unconfined , depending on the existence of a water table, defined by levels in shallow wells. ๏ƒ˜ A confined aquifer is one that is overlain by a confining unit and is under pressure. ๏ƒ˜ A leaky confined aquifer represents a stratum that allows water to flow from above through the confining zone. ๏ƒ˜ A perched water table is an example where an unconfined water body sits on top of a clay lens, separated from the main aquifer below.

๏ƒ˜ If the water level rises above the land surface, a flowing well or spring results and is referred to as an artesian well. ๏ƒ˜ The piezometric surface (potentiometric surface) of a confined aquifer is the hydrostatic pressure level of water in the aquifer, defined by the water level that occurs in a lined penetrating well. ๏ƒ˜ Contour maps and profiles can be prepared of the water table for an unconfined aquifer or the piezometric surface for a confined aquifer. These equipotential lines are lines of constant head. ๏ƒ˜ The hydraulic conductivity of a soil or rock depends on a variety of physical factors and is an indication of an aquiferโ€™s ability to transmit water. ๏ƒ˜ Transmissivity is a term often used in ground water hydraulics as applied to confined aquifers. ๏ƒ˜ The intrinsic permeability of a rock or soil is a property of the medium only, independent of fluid properties. ๏ƒ˜ The hydraulic conductivity , a measure of the ability of the porous media to transmit water. ๏ƒ˜ The slug test for shallow wells operates based on a measurement of decline or recovery of the water level in the well through time. Either the well can be pumped to lower the water level, and allowed to recover in time, or the water level can be increased and allowed to drain out in time. ๏ƒ˜ Hydraulic K is then determined by evaluating the rate of change in the water level with time. ๏ƒ˜ The pump test involves the constant removal of water from a single well and observations of water-level declines at several adjacent wells. In this way, an integrated K value for a portion of the aquifer is obtained. ๏ƒ˜ Tracer tests involve the injection of inorganic (chloride or bromide tracers) or organic chemicals into a well and the temporal measurement of concentration changes in wells positioned in the direction of ground water flow. ๏ƒ˜ Average seepage velocities can be determined by analyzing the breakthrough curves of tracer from the downgradient wells.

2. Why is ground water hydrology important to study?

Ground water hydrology is of great importance because of the use of aquifer systems for water supply and because of the threat of contamination from waste sites at or below the ground surface. Recent attention has focused on ground water contamination problems associated with industrial or chemical spills and leaks. Properties of the porous media and subsurface geology govern both the rate and direction of ground water flow in any aquifer system. The injection or accidental spill of waste into an aquifer or the pumping of the aquifer for water supply may alter the natural hydraulic flow patterns. The hydrologist must have a working knowledge of methods that have been developed to predict rates of flow and directions of movement in ground water systems. Only then can one possibly address problems of ground water contamination. Ground water is an important source of water supply for municipalities, agriculture, and industry. Techniques for the design of water supply systems that rely in part on ground water aquifers are an important part of engineering hydrology.