「ground-water」の共起表現(2語左で並び替え)

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共起表現

「ground-water」の共起表現一覧(2語左で並び替え)

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A major	groundwater plume containing the contaminant PCE was di
coming into contact with abundant, shallow	groundwater or surface water.
power line, receiving acidic, low-nutrient	groundwater.
area have been similarly badly affected by	groundwater pollution and other toxic emissions.
a primary cause for the increased amount of	groundwater in the lowlands.
n exposure to contaminants and contaminated	groundwater migration are under control.
e of an hydrogeological water balance and a	groundwater model (e.g.
ordane adheres to soil particles and enters	groundwater only slowly owing to its low solubility (0.
rocarbons in oil and gas reservoirs, and of	groundwater in aquifers.
lorida's the Brooksville Ridge and protects	groundwater recharge.
into the earth by infiltration and becomes	groundwater, much of which eventually enters streams.
metre clay cap over the site, and extensive	groundwater and soil vapour monitoring, testing and rep
ation of the mix of these chemicals and the	groundwater.
educing the runoff from a site and allowing	groundwater recharge.
dissolved substances from soil and shallow	groundwater can be flushed into streams.
ervoir storage, crop growth and irrigation,	groundwater flow, reach routing, nutrient and pesticide
ous acidic environments and Tharsis-centric	groundwater discharge dating to the late Noachian, much
ude environmental degradation and declining	groundwater.
ponsible for contaminating the soil and the	groundwater with three old hazardous-waste disposal are
Hexazinone is a known and pervasive	groundwater contaminant, due to its high water solubili
minating rainwater infiltration and natural	groundwater recharge.
efits in treating, restoring and recharging	groundwater.
ure or lies in deep underground aquifers as	groundwater not accessible to human use.
n oxide adsorption treatment for arsenic in	groundwater is a commonly practiced removal process whi
hat an ice storm formed the hole and as the	groundwater rose, the lake was created.
It acts as a	groundwater recharge zone for the Duffins Creek watersh
ota and Prince Edward Island, as well as in	groundwater in Long Island, New York and Florida.
As the	groundwater enters the cave, the excess carbon dioxide
water stream from sources such as brackish	groundwater.
subsurface characteristics (such as natural	groundwater velocity during ambient conditions, hydraul
rom the mountains, as well as supplementary	groundwater; owing to the lesser use of water to irriga
ted due to coastal sinking, associated with	groundwater withdrawal.
In addition to the association of	groundwater availability with this locale along the Bal
duced surface water availability, increased	groundwater inflow, water logging, polluted incoming wa
es - Investigating and raising awareness of	groundwater and water resource issues in Australia
Scientists believe that	groundwater sapping created these gullies in Noachis Te
on top of clay compact the clay beneath as	groundwater is drawn down and water is wrung out of the
water (arguably the largest single body of	groundwater in the world, although the overall volume o
The wells brought fresh	groundwater to farmers and others who previously had be
In hydrogeology it is measured by the	Groundwater flow equation.
The system is supplemented by four	groundwater waterworks on the North German Plain.
It is endemic to caves and	groundwater in Australia.
tain future, being threatened by changes in	groundwater quality and level, changes in aquifer chara
tically alters the acidity and chemistry of	groundwater and streams, and may endanger plant and ani
nd cavities by circulation of chloride rich	groundwater or connate fluids.
Using one of several classification of	groundwater based on Total Dissolved Solids, brine is w
The combination of	groundwater pumping for power production and water extr
he aquifer, to determine what is coming in (	groundwater recharge from the surface), what is leaving
ation) to achieve geochemical conditions in	groundwater that favor the growth of the dechlorinating
It should not be confused with	groundwater flow.
a specific wetland can be connected through	groundwater to other wetlands or lakes, or through surf
inhalation or ingestion of contaminants in	groundwater contaminated through soil.
eated landfills which have contaminated the	groundwater on Saipan, which could lead to disease.
r table to keep them from contaminating the	groundwater.
to the problem of arsenic contamination of	groundwater in Eastern India and Bangladesh.
generalization is arsenic contamination of	groundwater, as arsenic is a very serious pollutant whi
ants to surface water) and contamination of	groundwater, and to maintain and/or improve the conditi
Reclamation and provides flood control and	groundwater recharge of the aquifer.
,000,000 US gallons (380,000 m3) per day of	groundwater for public water use, industrial supply, an
Note that in fields that commonly deal with	groundwater chemistry, arsenite commonly refers to As2O
arce that there has been a rapid decline of	groundwater level in large parts of the Ghouta.
tics of the countries bedrock, deposits and	groundwater.
investigation found that shallow depths of	groundwater were contaminated.
ces of benzene and toluene were detected in	groundwater monitoring bores.
ellite images for both detecting subsurface	groundwater accumulation and land / submarine springs u
re at the facility, but has determined that	groundwater contamination is not under control.
ks due to their solubility in dilute acidic	groundwater.
pool can allow raw sewage to directly enter	groundwater with minimal biological cleansing, leading
ther water activities such as discharges to	groundwater, discharges to surface water, abstractions,
Calcite can be either dissolved by	groundwater or precipitated by groundwater, depending o
permeability properties or the distance to	groundwater -- but on other, less tangible criteria, in
The company diversified into	groundwater software training and consulting services,
m of a lengthy root system reaching down to	groundwater.
ng pit walls generate acid rock drainage in	groundwater, seeps, and surface water.
Farmers had been drinking fresh	groundwater from wells, whereas previously they had had
Baseflow (also called drought flow,	groundwater recession flow,, low flow, low-water flow,
The statue is currently leaning due to	groundwater level changes causing movement of the found
tial within the rocks and soils; and e) the	groundwater aquifers that contain groundwater resources
Not all ecosystems need	groundwater, of course.
tation watered by waterfalls emanating from	groundwater emerging from the upper cliff faces.
stems in more hospitable environments where	groundwater plays no central role, groundwater is in fa
If the inflow to the reservoir exceeds the	groundwater recharge capacity of the spreading grounds
t, which increased runoff at the expense of	groundwater.
e sources of water were explored, including	groundwater and rivers, but none were considered adequa
reater risks lie in soil vapor exposure and	groundwater contamination.
wers results in a significant extraction of	groundwater from the Ogallala Aquifer.
is slower than throughflow but faster than	groundwater flow.
3 past the Ship Pond Road bridge, is fed by	groundwater and has over two miles (3 km) of shoreline.
The pond is fed by	groundwater and cranberry bog outlets.
These kettleholes are fed by	groundwater and have no inlet streams.
It is fed by	groundwater and supply pipe of the near Taxer spring.
's crust, especially oil and gas fields and	groundwater aquifers.
of the Quincy Mine have slowly filled with	groundwater since the closing of the mine.
districts that is responsible for managing	groundwater and surface water resources in a 15-county
., Edgett, Kenneth S., "Evidence for Recent	Groundwater Seepage and Surface Runoff on Mars".
book of his recent work is forthcoming with	Groundwater Press.
This form of arsenate is often found in	groundwater from deep wells and is a toxic substance.
solate the processing area from surrounding	groundwater.
to remove arsenic from arsenic-contaminated	groundwater.
rocessing area is isolated from surrounding	groundwater by creating fractured areas ("pockets"), ap
It was isolated by Zhang et al. from a	groundwater sample in Japan.
e river draws its water mainly from natural	groundwater springs, snow melt, and rain water.
stance heating to vaporize the TCE from the	groundwater.
me-was the first fully-integrated graphical	groundwater modelling software.
canyon, or on the edge of a grassland where	groundwater bubbles to the surface.
lcite mineralization and tufa growth around	groundwater seepages.
tetrachloroethylene which had contaminated	groundwater.
Also, 'Gotjawal' has abundant	groundwater and excellent effects of heat-retaining and
enery along the base of the hills, captures	groundwater that nurtures the palms.
rface runoff from adjacent hillslopes, from	groundwater flow out of the ground, and from water disc
de and trichloroethene were detected in the	groundwater on the plant, but were only detected in lim
ary fringe is the subsurface layer in which	groundwater seeps up from a water table by capillary ac
corrosion of iron and steel in oxygen-free	groundwater and in reducing soils below the water table
when contaminants, either dissolved in the	groundwater or as DNAPL, come into contact with the iro
, after an epidemic of typhoid found in the	groundwater supply.
In A,	groundwater flows through the barrier and is remediated
islative accomplishments of his include the	Groundwater Protection Act (1983), California Clean Air
als; a situation explained by the inflow of	groundwater from an area larger than suggested by the e
osive because basaltic magma interacts with	groundwater in aquifers below the surface producing vio
of crustaceans which live interstitially in	groundwater.
stormwater though permeable soils into the	groundwater aquifer.
t pollution from the plant leached into the	groundwater and caused increased rates of cancer amongs
stormwater though permeable soils into the	groundwater aquifer.
not been cleared, and are seeping into the	groundwater.
stormwater though permeable soils into the	groundwater aquifer.
to the raised watertable below and into the	groundwater supply.
-rich mineral deposit became inundated with	groundwater that acted as a neutron moderator, and a nu
o used to regulate flows for irrigation and	groundwater recharge.
The river provides water for irrigation and	groundwater recharge.
Light Non-Aqueous Phase Liquid (LNAPL) is a	groundwater contaminate that is not soluble and has a l
(Darcy's law of	groundwater flow)
However, leaching and	groundwater leakage still causes some pollution.
It is used to reduce contaminant levels in	groundwater.
In some cases it requires the lowering of	groundwater levels below the level of the oil shale str
natural in- and outflow and mainly receives	groundwater of the Inn River and from rain.
ers of North America, where the majority of	groundwater chemistry data has been acquired.
s to the Wakulla River and St. Marks River,	groundwater, springs, sinkholes, wetlands, forests, and
ors, and unstable building material allowed	groundwater from the Nile to seep into the walls, causi
n 64,900 cubic kilometres (15,600 cu mi) of	groundwater.
f historic mining waste and $100 million on	groundwater cleanup.
uses both the GIS and Hydrologic model for	groundwater exploration in the northern United Arab Emi
icated; new users generally do not purchase	groundwater rights until they are sure they cannot obta
Officials said the leak did not contaminate	groundwater.
They receive their nutrients through	groundwater infiltration.
Biofouling can also occur in	groundwater wells where build-up can limit recovery flo
ence here may be due to upwellings of fresh	groundwater high in calcium carbonate.
Overdrafting is the process of extracting	groundwater beyond the safe yield or equilibrium yield
eam is contaminated from the mixture of the	groundwater and surface streams due to mining.
h frequent saline water degeneration of the	groundwater flow.
is important for bioremediation of polluted	groundwater.
when concerns arose about the status of the	groundwater aquifers which sat under the reservation.
U.S. gallons (1 billion m3) of contaminated	groundwater as a result of the leaks.
There is such an absence of usable	groundwater in the area that Eunice, N.M., the closest
This vector describes the direction of the	groundwater flow, where negative values indicate flow a
trol Board has indicated MTBE is one of the	groundwater pollutants of most widespread concern in th
avajo Aquifer is the main source of potable	groundwater for the Navajo and Hopi tribes, who use the
as well as a limited amount of contaminated	groundwater.
rea, thus facilitating recharge of precious	groundwater supplies locally.
mm)) characterized by the presence of both	groundwater and relatively nutrient-poor windblown sand
Because of falling	groundwater surrounding forests are dying.
xic materials caused contamination of local	groundwater.
in threat to its existence is loss of local	groundwater.
Normally, the removal of the	groundwater would have caused the collapse of the build
The uranium mining caused some of the	groundwater in Fry Canyon to become radioactive.
a depth of 3,800 feet, were turned off, and	groundwater from the surrounding aquifers began to slow
It focused on protecting	groundwater, which many residents surveyed had expresse
, due to the impact of mining on underlying	groundwater.
rite can result from hydrothermal or direct	groundwater precipitation.
The Jandakot Mound, or Jandakot	Groundwater Mound, is an unconfined aquifer in south-we
Fossil water or paleowater is	groundwater that has remained sealed in an aquifer for
oaches to application of iron particles for	groundwater remediation: Fig. A, a conventional PRB mad
ceeded, then negligible water percolates to	groundwater.
The source for this pond is	groundwater, and there is no outlet.
tension, detect deep and poorly accessible	groundwater resources, improve understanding of the evo
e for sites where there is a possibility of	groundwater contamination, or where there is soil with
s tebuthiuron to have a great potential for	groundwater contamination, due to its high water solubi
It may also be precipitated by	groundwater or in other sedimentary conditions, or form
g of waters (such as from precipitation and	groundwater) and the level of groundwater contribution
converts 1,2-DCE to VC, and its presence in	groundwater may be necessary for proper bioremediation
ilities for managing and protecting certain	groundwater resources within Alameda County.
r soil qualities and the close proximity to	groundwater with the engineering design of their "state
quently used for water quality improvement,	groundwater recharge, flood protection, aesthetic impro
ns, and thus can render large quantities of	groundwater non-potable.
e electromagnetic technology to rapidly map	groundwater in 3D deep beneath arid basins .
appened when the magmatic plume reached the	groundwater level of the Rhine (about 50m higher than t
ws a downward grade from its recharge zone,	groundwater can become pressurized as it flows.
le will seep into the soil and recharge the	groundwater aquifer.
to seep into the streambed, recharging the	groundwater aquifer.
ion for those within disciplines related to	groundwater, its occurrence, utilization, testing and m
reach there is a large historic release to	groundwater of solvent from manufacturing uses stemming
al cleaning and has been shown to remain in	groundwater for a long time if leaked.
pacted concrete dam, built to replenish the	groundwater supply to the Callide Irrigation area.
l Water Quality Control Board reported that	groundwater monitoring at the site had detected 26 vola
e as 1989, DBCP persistence was reported in	groundwater that was previously used for beneficial pur
Cambridge, Massachusetts doing research in	Groundwater modeling) and the Jawaharlal Nehru Fellowsh
As a result the	groundwater flow is diverted around the tailings.
below surface the Maroota Sand was rich in	groundwater.
d continuous rainfall on site; and rises in	groundwater.
their useful life is over or when a risk of	groundwater contamination arises.
and reliable chemical indicator of river /	groundwater fecal contamination, as chloride is a non-r

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共起表現

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「ground-water」の共起表現一覧(2語左で並び替え)