「ground-water」の共起表現(1語左で並び替え)

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共起表現

「ground-water」の共起表現一覧(1語左で並び替え)

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The system was changed over to a	groundwater well source, dramatically improving water q
e of an hydrogeological water balance and a	groundwater model (e.g.
It acts as a	groundwater recharge zone for the Duffins Creek watersh
Light Non-Aqueous Phase Liquid (LNAPL) is a	groundwater contaminate that is not soluble and has a l
It was isolated by Zhang et al. from a	groundwater sample in Japan.
In A,	groundwater flows through the barrier and is remediated
Also, 'Gotjawal' has abundant	groundwater and excellent effects of heat-retaining and
tension, detect deep and poorly accessible	groundwater resources, improve understanding of the evo
ks due to their solubility in dilute acidic	groundwater.
ors, and unstable building material allowed	groundwater from the Nile to seep into the walls, causi
educing the runoff from a site and allowing	groundwater recharge.
g of waters (such as from precipitation and	groundwater) and the level of groundwater contribution
Regular monitoring of soil and	groundwater around manure holding facilities and land r
o used to regulate flows for irrigation and	groundwater recharge.
Reclamation and provides flood control and	groundwater recharge of the aquifer.
on Agency have identified numerous soil and	groundwater contaminants on and near the development ar
jor contaminants in the soil, sediment, and	groundwater are volatile organic compounds (VOCs), poly
tics of the countries bedrock, deposits and	groundwater.
r buildings will be dismantled and soil and	groundwater will be decontaminated.
's crust, especially oil and gas fields and	groundwater aquifers.
nding the fate and transport of surface and	groundwater pollutants.
chloride, were extracted from the soil and	groundwater.
nflow and infiltration of surface water and	groundwater, which can lead to sanitary sewer overflows
on Reduction Potential or redox in soil and	groundwater, together with pH, temperature, oxygen cont
d hydrophobic organic compounds in soil and	groundwater.
It is endemic to caves and	groundwater in Australia.
er waste handling and removal, the soil and	groundwater beneath the property became contaminated an
The river provides water for irrigation and	groundwater recharge.
At sites where soil and	groundwater are contaminated with chlorinated ethenes,
em at the waste pond, freezing the soil and	groundwater to a depth of approximately 30 feet (9.1 m)
However, leaching and	groundwater leakage still causes some pollution.
a depth of 3,800 feet, were turned off, and	groundwater from the surrounding aquifers began to slow
es through soil, polluting both surface and	groundwater.
ruptions; the application of soil, rock and	groundwater mechanics to the design and predicted perfo
The soil and	groundwater of the site was contaminated during operati
e tanks have leaked waste into the soil and	groundwater.
ues have persisted in contaminated soil and	groundwater long after applications have ceased.
reater risks lie in soil vapor exposure and	groundwater contamination.
Area	groundwater, which is the principal source of water sup
lcite mineralization and tufa growth around	groundwater seepages.
to remove arsenic from arsenic-contaminated	groundwater.
e forests provide several functions such as	groundwater recharge, water quality enhancement through
on top of clay compact the clay beneath as	groundwater is drawn down and water is wrung out of the
ure or lies in deep underground aquifers as	groundwater not accessible to human use.
heavy metals from the slag heaps as well as	groundwater and surface runoff from the metal smelters
hing land use, and to find a way to balance	groundwater withdrawals and discharges.
into the earth by infiltration and becomes	groundwater, much of which eventually enters streams.
more generally called a hydrograph (in both	groundwater and surface water).
mm)) characterized by the presence of both	groundwater and relatively nutrient-poor windblown sand
water stream from sources such as brackish	groundwater.
heads typical of valley features shaped by	groundwater sapping.
It may also be precipitated by	groundwater or in other sedimentary conditions, or form
3 past the Ship Pond Road bridge, is fed by	groundwater and has over two miles (3 km) of shoreline.
area have been similarly badly affected by	groundwater pollution and other toxic emissions.
The pond is fed by	groundwater and cranberry bog outlets.
Calcite can be either dissolved by	groundwater or precipitated by groundwater, depending o
These kettleholes are fed by	groundwater and have no inlet streams.
It is fed by	groundwater and supply pipe of the near Taxer spring.
enery along the base of the hills, captures	groundwater that nurtures the palms.
e freeze wall these methods can still cause	groundwater contamination as the hydraulic conductivity
ilities for managing and protecting certain	groundwater resources within Alameda County.
lly untreated sewage injected to the city's	groundwater.
Cold	groundwater will be pumped up from within the earth and
Officials said the leak did not contaminate	groundwater.
tetrachloroethylene which had contaminated	groundwater.
n exposure to contaminants and contaminated	groundwater migration are under control.
U.S. gallons (1 billion m3) of contaminated	groundwater as a result of the leaks.
to ensure no one is exposed to contaminated	groundwater.
as well as a limited amount of contaminated	groundwater.
rtiary butyl ether (MTBE) was contaminating	groundwater.
The very cool	groundwater running into the sea keeps the sea fresh al
Cooling	groundwater or mixing of different groundwaters will al
g half-life of 36Cl makes it useful to date	groundwater up to one million years old.
ude environmental degradation and declining	groundwater.
Deep	groundwater is fed to the creek by the Black Creek aqui
rite can result from hydrothermal or direct	groundwater precipitation.
pool can allow raw sewage to directly enter	groundwater with minimal biological cleansing, leading
otal of £54,000 for causing petrol to enter	groundwater and a tributary of the Foudry Brook, from i
ordane adheres to soil particles and enters	groundwater only slowly owing to its low solubility (0.
Since every	groundwater basin recharges at a different rate dependi
metre clay cap over the site, and extensive	groundwater and soil vapour monitoring, testing and rep
Overdrafting is the process of extracting	groundwater beyond the safe yield or equilibrium yield
ndenburger Tor was delayed owing to extreme	groundwater problems at the site of the latter new stat
Because of falling	groundwater surrounding forests are dying.
fed by, and (at other places or times) feed	groundwater, to varying degrees.
Baseflow (also called drought flow,	groundwater recession flow,, low flow, low-water flow,
e of the claimed derogation of river flows,	groundwater abstractions and local springs due to histo
d dynamics, Land for hydrology and Soil for	groundwater flow.
s tebuthiuron to have a great potential for	groundwater contamination, due to its high water solubi
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
oaches to application of iron particles for	groundwater remediation: Fig. A, a conventional PRB mad
he lower part of the river is only used for	groundwater recharge.
The system is supplemented by four	groundwater waterworks on the North German Plain.
ence here may be due to upwellings of fresh	groundwater high in calcium carbonate.
The wells brought fresh	groundwater to farmers and others who previously had be
Farmers had been drinking fresh	groundwater from wells, whereas previously they had had
ed, 317, 289, 374 and 357 Mm3 of water from	groundwater resources of the city.
tation watered by waterfalls emanating from	groundwater emerging from the upper cliff faces.
rface runoff from adjacent hillslopes, from	groundwater flow out of the ground, and from water disc
collected specimens of P. subterraneus from	groundwater at his farm near Eyreton, Canterbury, and l
me-was the first fully-integrated graphical	groundwater modelling software.
high	groundwater levels, close to the infiltrating surface;
Hinkley	groundwater contamination
quently used for water quality improvement,	groundwater recharge, flood protection, aesthetic impro
This form of arsenate is often found in	groundwater from deep wells and is a toxic substance.
converts 1,2-DCE to VC, and its presence in	groundwater may be necessary for proper bioremediation
The contents of dissolved solids in	groundwater vary highly from one location to another on
below surface the Maroota Sand was rich in	groundwater.
ota and Prince Edward Island, as well as in	groundwater in Long Island, New York and Florida.
ng pit walls generate acid rock drainage in	groundwater, seeps, and surface water.
Biofouling can also occur in	groundwater wells where build-up can limit recovery flo
inhalation or ingestion of contaminants in	groundwater contaminated through soil.
al cleaning and has been shown to remain in	groundwater for a long time if leaked.
ces of benzene and toluene were detected in	groundwater monitoring bores.
e as 1989, DBCP persistence was reported in	groundwater that was previously used for beneficial pur
It is used to reduce contaminant levels in	groundwater.
ation) to achieve geochemical conditions in	groundwater that favor the growth of the dechlorinating
tain future, being threatened by changes in	groundwater quality and level, changes in aquifer chara
Cambridge, Massachusetts doing research in	Groundwater modeling) and the Jawaharlal Nehru Fellowsh
n oxide adsorption treatment for arsenic in	groundwater is a commonly practiced removal process whi
he aquifer, to determine what is coming in (	groundwater recharge from the surface), what is leaving
d continuous rainfall on site; and rises in	groundwater.
of crustaceans which live interstitially in	groundwater.
e sources of water were explored, including	groundwater and rivers, but none were considered adequa
duced surface water availability, increased	groundwater inflow, water logging, polluted incoming wa
The company diversified into	groundwater software training and consulting services,
ervoir storage, crop growth and irrigation,	groundwater flow, reach routing, nutrient and pesticide
Fossil water or paleowater is	groundwater that has remained sealed in an aquifer for
The source for this pond is	groundwater, and there is no outlet.
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
trates into the ground recharging the local	groundwater, because the water table is below the botto
nity for their water pollution of the local	groundwater with toxic chemicals, such as solvents and
xic materials caused contamination of local	groundwater.
in threat to its existence is loss of local	groundwater.
power line, receiving acidic, low-nutrient	groundwater.
A major	groundwater plume containing the contaminant PCE was di
districts that is responsible for managing	groundwater and surface water resources in a 15-county
e electromagnetic technology to rapidly map	groundwater in 3D deep beneath arid basins .
dy to determine how to restore the Milltown	groundwater.
has risen to within 150 feet of the natural	groundwater level.
subsurface characteristics (such as natural	groundwater velocity during ambient conditions, hydraul
e river draws its water mainly from natural	groundwater springs, snow melt, and rain water.
minating rainwater infiltration and natural	groundwater recharge.
Not all ecosystems need	groundwater, of course.
raction of water from such non-replenishing	groundwater reserves (known as low safe-yield reserves)
The use of	groundwater drains has been suggested by hydrologist Dr
ns, and thus can render large quantities of	groundwater non-potable.
ers of North America, where the majority of	groundwater chemistry data has been acquired.
nformation exchange related to the study of	groundwater.
tically alters the acidity and chemistry of	groundwater and streams, and may endanger plant and ani
a primary cause for the increased amount of	groundwater in the lowlands.
es - Investigating and raising awareness of	groundwater and water resource issues in Australia
,000,000 US gallons (380,000 m3) per day of	groundwater for public water use, industrial supply, an
rocarbons in oil and gas reservoirs, and of	groundwater in aquifers.
n 64,900 cubic kilometres (15,600 cu mi) of	groundwater.
The volume of	groundwater extracted from the catchment has fallen in
to the problem of arsenic contamination of	groundwater in Eastern India and Bangladesh.
Using one of several classification of	groundwater based on Total Dissolved Solids, brine is w
t, which increased runoff at the expense of	groundwater.
arce that there has been a rapid decline of	groundwater level in large parts of the Ghouta.
their useful life is over or when a risk of	groundwater contamination arises.
The use of	groundwater as a source of renewable energy will greatl
In some cases it requires the lowering of	groundwater levels below the level of the oil shale str
e for sites where there is a possibility of	groundwater contamination, or where there is soil with
wers results in a significant extraction of	groundwater from the Ogallala Aquifer.
generalization is arsenic contamination of	groundwater, as arsenic is a very serious pollutant whi
(Darcy's law of	groundwater flow)
ants to surface water) and contamination of	groundwater, and to maintain and/or improve the conditi
investigation found that shallow depths of	groundwater were contaminated.
water (arguably the largest single body of	groundwater in the world, although the overall volume o
In addition to the association of	groundwater availability with this locale along the Bal
er operations, exploring conjunctive use of	groundwater and surface water, evaluating and improving
The combination of	groundwater pumping for power production and water extr
Protection Agency stated that many years of	groundwater testing surrounding the landfill indicated
als; a situation explained by the inflow of	groundwater from an area larger than suggested by the e
f historic mining waste and $100 million on	groundwater cleanup.
revent infiltration of chemicals to soil or	groundwater.
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
corrosion of iron and steel in oxygen-free	groundwater and in reducing soils below the water table
Hexazinone is a known and pervasive	groundwater contaminant, due to its high water solubili
soil particles and can continue to pollute	groundwater for years after its application.
is important for bioremediation of polluted	groundwater.
avajo Aquifer is the main source of potable	groundwater for the Navajo and Hopi tribes, who use the
rea, thus facilitating recharge of precious	groundwater supplies locally.
mbrella" of bitumen-coated paper to prevent	groundwater from seeping into the station.
l legislation to preserve wetlands, protect	groundwater quantity and quality, strengthen air qualit
It focused on protecting	groundwater, which many residents surveyed had expresse
lorida's the Brooksville Ridge and protects	groundwater recharge.
icated; new users generally do not purchase	groundwater rights until they are sure they cannot obta
natural in- and outflow and mainly receives	groundwater of the Inn River and from rain.
., Edgett, Kenneth S., "Evidence for Recent	Groundwater Seepage and Surface Runoff on Mars".
g in water that percolates down to recharge	groundwater.
efits in treating, restoring and recharging	groundwater.
Relative	groundwater travel times.
nd cavities by circulation of chloride rich	groundwater or connate fluids.
s to the Wakulla River and St. Marks River,	groundwater, springs, sinkholes, wetlands, forests, and

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「ground-water」の共起表現一覧(1語左で並び替え)