「ground water」の共起表現(1語右で並び替え)

「ground water」の共起表現一覧(1語右で並び替え)

ground water

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1語右で並び替え

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e of the claimed derogation of river flows, groundwater abstractions and local springs due to histo
ellite images for both detecting subsurface groundwater accumulation and land / submarine springs u
g of waters (such as from precipitation and groundwater) and the level of groundwater contribution
tically alters the acidity and chemistry of groundwater and streams, and may endanger plant and ani
eam is contaminated from the mixture of the groundwater and surface streams due to mining.
more generally called a hydrograph (in both groundwater and surface water).
es - Investigating and raising awareness of groundwater and water resource issues in Australia
t pollution from the plant leached into the groundwater and caused increased rates of cancer amongs
in mobility and availability of uranium to groundwater and soil from nuclear wastes which leads to
corrosion of iron and steel in oxygen-free groundwater and in reducing soils below the water table
es, extinct plant and animal species, toxic groundwater, and increased flooding.
districts that is responsible for managing groundwater and surface water resources in a 15-county
e sources of water were explored, including groundwater and rivers, but none were considered adequa
heavy metals from the slag heaps as well as groundwater and surface runoff from the metal smelters
metre clay cap over the site, and extensive groundwater and soil vapour monitoring, testing and rep
3 past the Ship Pond Road bridge, is fed by groundwater and has over two miles (3 km) of shoreline.
mm)) characterized by the presence of both groundwater and relatively nutrient-poor windblown sand
ants to surface water) and contamination of groundwater, and to maintain and/or improve the conditi
cidentally infiltrate some of its volume to groundwater); and from a retention basin, which is desi
The pond is fed by groundwater and cranberry bog outlets.
er operations, exploring conjunctive use of groundwater and surface water, evaluating and improving
These kettleholes are fed by groundwater and have no inlet streams.
otal of £54,000 for causing petrol to enter groundwater and a tributary of the Foudry Brook, from i
Also, 'Gotjawal' has abundant groundwater and excellent effects of heat-retaining and
are design to withstand site specific soil, groundwater and traffic loading conditions provide valu
It is fed by groundwater and supply pipe of the near Taxer spring.
The source for this pond is groundwater, and there is no outlet.
stormwater though permeable soils into the groundwater aquifer.
stormwater though permeable soils into the groundwater aquifer.
le will seep into the soil and recharge the groundwater aquifer.
to seep into the streambed, recharging the groundwater aquifer.
stormwater though permeable soils into the groundwater aquifer.
when concerns arose about the status of the groundwater aquifers which sat under the reservation.
tial within the rocks and soils; and e) the groundwater aquifers that contain groundwater resources
's crust, especially oil and gas fields and groundwater aquifers.
jor contaminants in the soil, sediment, and groundwater are volatile organic compounds (VOCs), poly
At sites where soil and groundwater are contaminated with chlorinated ethenes,
Regular monitoring of soil and groundwater around manure holding facilities and land r
U.S. gallons (1 billion m3) of contaminated groundwater as a result of the leaks.
The use of groundwater as a source of renewable energy will greatl
generalization is arsenic contamination of groundwater, as arsenic is a very serious pollutant whi
collected specimens of P. subterraneus from groundwater at his farm near Eyreton, Canterbury, and l
at are inundated or saturated by surface or groundwater at a frequency and duration sufficient to s
at are inundated or saturated by surface or groundwater at a frequency and duration sufficient to s
In addition to the association of groundwater availability with this locale along the Bal
Using one of several classification of groundwater based on Total Dissolved Solids, brine is w
Since every groundwater basin recharges at a different rate dependi
trates into the ground recharging the local groundwater, because the water table is below the botto
er waste handling and removal, the soil and groundwater beneath the property became contaminated an
Overdrafting is the process of extracting groundwater beyond the safe yield or equilibrium yield
canyon, or on the edge of a grassland where groundwater bubbles to the surface.
rocessing area is isolated from surrounding groundwater by creating fractured areas ("pockets"), ap
ws a downward grade from its recharge zone, groundwater can become pressurized as it flows.
dissolved substances from soil and shallow groundwater can be flushed into streams.
Groundwater can either be privately owned or publicly o
ers of North America, where the majority of groundwater chemistry data has been acquired.
Note that in fields that commonly deal with groundwater chemistry, arsenite commonly refers to As2O
f historic mining waste and $100 million on groundwater cleanup.
Hexazinone is a known and pervasive groundwater contaminant, due to its high water solubili
on Agency have identified numerous soil and groundwater contaminants on and near the development ar
Light Non-Aqueous Phase Liquid (LNAPL) is a groundwater contaminate that is not soluble and has a l
inhalation or ingestion of contaminants in groundwater contaminated through soil.
re at the facility, but has determined that groundwater contamination is not under control.
their useful life is over or when a risk of groundwater contamination arises.
Hinkley groundwater contamination
e freeze wall these methods can still cause groundwater contamination as the hydraulic conductivity
s tebuthiuron to have a great potential for groundwater contamination, due to its high water solubi
e for sites where there is a possibility of groundwater contamination, or where there is soil with
reater risks lie in soil vapor exposure and groundwater contamination.
ous acidic environments and Tharsis-centric groundwater discharge dating to the late Noachian, much
ther water activities such as discharges to groundwater, discharges to surface water, abstractions,
The use of groundwater drains has been suggested by hydrologist Dr
Groundwater elevation is approximately at the elevation
tation watered by waterfalls emanating from groundwater emerging from the upper cliff faces.
As the groundwater enters the cave, the excess carbon dioxide
MT is also used for groundwater exploration and mapping, hydrocarbon reserv
uses both the GIS and Hydrologic model for groundwater exploration in the northern United Arab Emi
The volume of groundwater extracted from the catchment has fallen in
and reliable chemical indicator of river / groundwater fecal contamination, as chloride is a non-r
Groundwater feeds soil moisture through percolation, an
rface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water disc
Some groundwater flow occurs across this fault boundary, but
Groundwater flow is defined as the "...part of streamfl
In hydrogeology it is measured by the Groundwater flow equation.
2 gallons of precipitation per year, though groundwater flow is unknown.
As a result the groundwater flow is diverted around the tailings.
(Darcy's law of groundwater flow)
This vector describes the direction of the groundwater flow, where negative values indicate flow a
ervoir storage, crop growth and irrigation, groundwater flow, reach routing, nutrient and pesticide
h frequent saline water degeneration of the groundwater flow.
d dynamics, Land for hydrology and Soil for groundwater flow.
is slower than throughflow but faster than groundwater flow.
It should not be confused with groundwater flow.
In A, groundwater flows through the barrier and is remediated
,000,000 US gallons (380,000 m3) per day of groundwater for public water use, industrial supply, an
al cleaning and has been shown to remain in groundwater for a long time if leaked.
avajo Aquifer is the main source of potable groundwater for the Navajo and Hopi tribes, who use the
soil particles and can continue to pollute groundwater for years after its application.
elp understanding of formations which store groundwater for drinking or irrigation, and to help loc
This form of arsenate is often found in groundwater from deep wells and is a toxic substance.
mbrella" of bitumen-coated paper to prevent groundwater from seeping into the station.
Farmers had been drinking fresh groundwater from wells, whereas previously they had had
wers results in a significant extraction of groundwater from the Ogallala Aquifer.
ors, and unstable building material allowed groundwater from the Nile to seep into the walls, causi
a depth of 3,800 feet, were turned off, and groundwater from the surrounding aquifers began to slow
als; a situation explained by the inflow of groundwater from an area larger than suggested by the e
It emerged that the groundwater has been polluted since the 1970s.
ence here may be due to upwellings of fresh groundwater high in calcium carbonate.
osive because basaltic magma interacts with groundwater in aquifers below the surface producing vio
ion in the country and only plant that used groundwater in such a way.
a primary cause for the increased amount of groundwater in the lowlands.
rocarbons in oil and gas reservoirs, and of groundwater in aquifers.
to the problem of arsenic contamination of groundwater in Eastern India and Bangladesh.
ota and Prince Edward Island, as well as in groundwater in Long Island, New York and Florida.
There is such an absence of usable groundwater in the area that Eunice, N.M., the closest
e electromagnetic technology to rapidly map groundwater in 3D deep beneath arid basins .
It is endemic to caves and groundwater in Australia.
water (arguably the largest single body of groundwater in the world, although the overall volume o
The uranium mining caused some of the groundwater in Fry Canyon to become radioactive.
They receive their nutrients through groundwater infiltration.
duced surface water availability, increased groundwater inflow, water logging, polluted incoming wa
on top of clay compact the clay beneath as groundwater is drawn down and water is wrung out of the
While groundwater is a renewable source, reserves replenish r
Groundwater is scarce, and hikers generally rely on wat
n oxide adsorption treatment for arsenic in groundwater is a commonly practiced removal process whi
Deep groundwater is fed to the creek by the Black Creek aqui
ion for those within disciplines related to groundwater, its occurrence, utilization, testing and m
However, leaching and groundwater leakage still causes some pollution.
appened when the magmatic plume reached the groundwater level of the Rhine (about 50m higher than t
arce that there has been a rapid decline of groundwater level in large parts of the Ghouta.
The statue is currently leaning due to groundwater level changes causing movement of the found
bricklayers to build supporting walls, the groundwater level had to be lowered.
has risen to within 150 feet of the natural groundwater level.
In some cases it requires the lowering of groundwater levels below the level of the oil shale str
high groundwater levels, close to the infiltrating surface;
ues have persisted in contaminated soil and groundwater long after applications have ceased.
converts 1,2-DCE to VC, and its presence in groundwater may be necessary for proper bioremediation
Groundwater may have existed at both Gusev and Meridian
ruptions; the application of soil, rock and groundwater mechanics to the design and predicted perfo
n exposure to contaminants and contaminated groundwater migration are under control.
e of an hydrogeological water balance and a groundwater model (e.g.
Cambridge, Massachusetts doing research in Groundwater modeling) and the Jawaharlal Nehru Fellowsh
me-was the first fully-integrated graphical groundwater modelling software.
c. (WHI) is a company that specializes with groundwater modelling software, training, and consultin
ces of benzene and toluene were detected in groundwater monitoring bores.
l Water Quality Control Board reported that groundwater monitoring at the site had detected 26 vola
The lake lies on the Jandakot Groundwater Mound - a region of elevated groundwater be
The Jandakot Mound, or Jandakot Groundwater Mound, is an unconfined aquifer in south-we
into the earth by infiltration and becomes groundwater, much of which eventually enters streams.
dies, paid for by Rohm and Haas, showed the groundwater never affected the town's well water.
ns, and thus can render large quantities of groundwater non-potable.
ure or lies in deep underground aquifers as groundwater not accessible to human use.
natural in- and outflow and mainly receives groundwater of the Inn River and from rain.
Not all ecosystems need groundwater, of course.
reach there is a large historic release to groundwater of solvent from manufacturing uses stemming
The soil and groundwater of the site was contaminated during operati
eated landfills which have contaminated the groundwater on Saipan, which could lead to disease.
de and trichloroethene were detected in the groundwater on the plant, but were only detected in lim
ordane adheres to soil particles and enters groundwater only slowly owing to its low solubility (0.
nd cavities by circulation of chloride rich groundwater or connate fluids.
It may also be precipitated by groundwater or in other sedimentary conditions, or form
coming into contact with abundant, shallow groundwater or surface water.
when contaminants, either dissolved in the groundwater or as DNAPL, come into contact with the iro
Calcite can be either dissolved by groundwater or precipitated by groundwater, depending o
Cooling groundwater or mixing of different groundwaters will al
rom the mountains, as well as supplementary groundwater; owing to the lesser use of water to irriga
stems in more hospitable environments where groundwater plays no central role, groundwater is in fa
ions with test wells, including the uranium groundwater plume extending south of the plant area, st
A major groundwater plume containing the contaminant PCE was di
trol Board has indicated MTBE is one of the groundwater pollutants of most widespread concern in th
nding the fate and transport of surface and groundwater pollutants.
area have been similarly badly affected by groundwater pollution and other toxic emissions.
rite can result from hydrothermal or direct groundwater precipitation.
book of his recent work is forthcoming with Groundwater Press.
ndenburger Tor was delayed owing to extreme groundwater problems at the site of the latter new stat
The USGS groundwater program had already determined that there w
islative accomplishments of his include the Groundwater Protection Act (1983), California Clean Air
he San Joaquin Valley of the United States, groundwater pumping for crops has gone on for generatio
Groundwater pumping continues at a higher rate than the
The combination of groundwater pumping for power production and water extr
tain future, being threatened by changes in groundwater quality and level, changes in aquifer chara
l legislation to preserve wetlands, protect groundwater quantity and quality, strengthen air qualit
s a moist or wet place where water, usually groundwater, reaches the earth's surface from an underg
Baseflow (also called drought flow, groundwater recession flow,, low flow, low-water flow,
It acts as a groundwater recharge zone for the Duffins Creek watersh
Reclamation and provides flood control and groundwater recharge of the aquifer.
If the inflow to the reservoir exceeds the groundwater recharge capacity of the spreading grounds
he aquifer, to determine what is coming in ( groundwater recharge from the surface), what is leaving
Groundwater recharge, which is an important process tha
quently used for water quality improvement, groundwater recharge, flood protection, aesthetic impro
e forests provide several functions such as groundwater recharge, water quality enhancement through
o used to regulate flows for irrigation and groundwater recharge.
lorida's the Brooksville Ridge and protects groundwater recharge.
educing the runoff from a site and allowing groundwater recharge.
The river provides water for irrigation and groundwater recharge.
minating rainwater infiltration and natural groundwater recharge.
he lower part of the river is only used for groundwater recharge.
oaches to application of iron particles for groundwater remediation: Fig. A, a conventional PRB mad
raction of water from such non-replenishing groundwater reserves (known as low safe-yield reserves)

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