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67 Cards in this Set

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Hydrologic cycle

This cycle includes the precipitation of water from clouds, infiltration into the ground or runoff into surface watercourses, followed by evaporation and transpiration of the water back into the atmosphere.

Evapotranspiration

The total water loss to the atmosphere by both evaporation and transpiration.

Transpiration

Water lost by plants

Percolation

When surface water (especially during a precipitation event) seeps into the ground and becomes groundwater.

Groundwater

Water within Zone of Saturation.

Zone of aeration

(Vadose zone) surface soil pore spaces contain both air and water.

Zone of saturation

Below the zone of Saturation, in which the pores are filled with water.

Water table

The surface of the saturated layer.

Aquifer

A stratum that contains a substantial amount of groundwater.

Unconfined aquifer

If a aquifer is underlain by an impervious stratum.

Confined aquifer

If the stratum containing water is trapped between two impervious layers.

Porosity

(Volume of voids)/(Total volume)

Artesian well

A well that is tapped into a confined aquifer under pressure.

Specific yield

The amount of water that can be extracted from a well.

Coefficient of permeability

A FUDGE factor, an indirect measure of the ability of a soil sample to transmit water.

Permeameter

consist of a soil sample through which a fluid is forced through, a Coefficient of permeability is calculated.

Cone of depression drawdown

a cone shape in the water table to a pump due to an increase velocity, loss of energy, and the energy gradient increasing.

Softening

removal of hardness

Hardness

caused by multivalent cations (or minerals) such as calcium, magnesium, and iron that dissolve from soil and rocks (particularly limestone). Causes scale and reduces the effectiveness of soap.

Carbonate hardness

Equal to the smaller of alkalinity or total hardness.

Non Carbonate hardness

Equal to the difference between total hardness and carbonate hardness.

Coagulation

Is the chemical alteration of the colloidal particles to make them stick together to form larger particles called flocs.

Flocculation

Assists in growth of larger particles in a physical process, stirring the liquid to increase velocity between particles and having them collide more often.

Coagulant

Chemicals that neutralize charges of particles and aid in making tiny particles sticky.

Floc

Larger particles made from coagulation.

Gravity settling

Allows heavier-than-water particles to settle to bottom.

Critical settling velocity

Overflow rate. The velocity a particle has to make it fall to bottom.

Overflow rate

fal/day-ft^3. Velocity of a critical particle.

Critical particle

particles with lower settling velocities are not all removed and particles with higher settling velocities are all removed.

Rapid sand filter

Fluid is run through a layer of sand, gravel and false floor.

Backwash

Cleans a Rapid sand filter

Filtration rate

Is the rate of water applied to the surface area of the filter.

CT

CT-concept; Adequate disinfection is a balance between the Concentration of the disinfectant © and the contact time (T), and analysis.

THM

The predominant DBPs are trihalomethanes.

DBP

disinfection byproducts formed from chlorine reacting with organic matter.

Chlorination

Treating water with Chlorine.

Fluoridation

Removal of fluoride removal.

Sanitary sewer

Large pipes flowing partially full (not under pressure).

Storm sewer

Sewers designed to capture storm water.

Nitrification

convert ammonia nitrogen to NO3-, nitrogen removal

Denitrification

remove nutrient properties of nitrogen, nitrate converted to nitrogen gas. Ammonia to nitrate, reduce nitrogen gas by facultative and anaerobic bacteria

Anoxic

sludge containing NO3 condition, microorganisms use nitrogen as electron acceptor.

condition, microorganisms use nitrogen as electron acceptor.

Phosphorous removal

accomplished by chemical or biological means, chemical requires phosphorus be fully oxidized. Chemical used for removal are lime and alum.

Luxury uptake

of phosphorus followed by removal of cells from liquid stream, removing phosphorus. Cells store phosphorus in cellular material.

Natural systems

Water systems cleaning water not man made

Lagoons

Large bodies of water with shallow depth

Stabilization ponds

consist of shallow man-made basins comprising a single or several series of anaerobic, facultative or maturation ponds. BOD removed. Facultative ponds

Surface flow wetlands

resemble natural, more common, free water surface, open water. Low permeability material (clay), bottom, avoid groundwater contamination.

Subsurface flow wetland

vegetated submerged bed, gravel/reed bed, replace septic systems, reduce mosquito and odor problems.

Primary solids

raw primary sludge, biological and secondary sludge.

Sludge stabilization

reduce problems associated with 2 of detrimental characteristics: sludge odor, putrescence, pathogenic organisms.

Lime stabilization

adding lime to sludge, raise pH to about 11 or up. Reduces odor, destroys pathogens, only temporary

Aerobic digestion

waste activate sludge placed in aeration tanks for long time, concentrated solids allowed to progress well into respiration phase. Net reduction in total and volatile solids.

Anaerobic digestion

dissolve organisms by extracellular enzymes

Acid formers

production of organic acids by a large group of anaerobic micro.

Methane formers

organic acids degraded further by a group of obligate anaerobes.

Sludge drying beds

dewatering, sand beds, cos-effective, consist tile drains in gravel covered by sand. Sludge dewatered poured on beds.

Gravity belt thickner

sludge introduced, free water drips through moving belt. Solids retained on surface of belt. Belt moves into dewatering zone.

Belt filter

operates as both a pressure filter and gravity filter.

Centrifuge

sludge placed into it, solids settle out by centrifugal force. Scraped out of bowl.

Centrate

decanted liquid from centrifuge

Cake

dewatered solids, discharged when belts separate. Solids coming out of centrifuge.

Filtrate

belt moves into dewatering zone, sludge squeezed between two belts, forced from sludge solids.

Dry adiabatic lapse rate

imaginary parcel of air rises through the atmosphere it experiences lower and lower pressure so it expands. The rate is the warming or cooling.

Troposphere

Troposphere: 5 km thick at poles, 18 km at equator. Temperature decreases with altitude. More than 80% of the mass of the atmosphere.

Stratosphere

Stratosphere: little mixing. Temperature profile inverted. High ozone concentration.

Mesosphere

Only 0.1% mass of air in layers above stratosphere