「ground-water」の共起表現(1語右で並び替え)

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共起表現

「ground-water」の共起表現一覧(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)

1 2 次へ＞

共起表現

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「ground-water」の共起表現一覧(1語右で並び替え)