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词汇 example_english_water-table
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Examples of water table


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
Depressions, or dolines, are fairly common, although cenotes open to the watertable are exceedingly rare in most of the study area.
Likewise, failure and success may not always be predicted by distance from the coast or depth of the watertable.
These changes he interpreted as a response to variations in watertable levels.
The watertable in the experimental site ranged from 1.2 to 1.4 m throughout the crop growth periods.
Because the watertable was below 2.0 m depth, the soil was medium textured, and the area was flat, capillary rise was ignored.
Nodulation occurred on tabular buttresses in horizontal lines just above the watertable level.
The nodules below the watertable showed a similar distribution of colour.
These gradual rises in the number of plant species reflect improved peat-forming conditions resulting from local rises of the watertable.
This is particularly suggested by the succession of evaporite couplets, which are attributed to pulsating episodes of watertable change.
The watertable had an average depth of 25 cm along the sampled radial segment and was visible in the depressions.
Both environmental changes could result in watertable changes fatal for survival of some plant species.
It is produced in the dry season, in areas with a high watertable or with irrigation, and in the rainy season.
In either case the toxic or radioactive waste is trapped in the solid, preventing it from leaching into the local watertable.
According to the relative abundance of legume species, possibilities for comparisons between plots, and watertable, representative species and individuals were chosen for nodulation studies.
Blocks with water extraction more than recharge indicate receding watertable zones.
The formation of inertinite-rich coals is generally related to peat oxidation due to watertable drop or fluctuation.
Many hand-dug wells went dry or became contaminated because of the sudden drop in the watertable.
This scramble, however, contributed to the further depletion of the already low watertable.
The knowledge of the local community about rainfall, watertable elevation, its spatial variability and hydrochemistry was compared with data from a hydrological monitoring program.
As an example, thin impure coal seams can form in places other than where a permanent watertable allows peat accumulation, even in semi-arid conditions.
These salts cannot be flushed because of the high watertable, hence the accumulation of saline lands in large-scale irrigation systems.
It is impossible to measure directly the acreage of land successfully drained and the incremental progression of the gradual lowering of the watertable.
Leaching through the subsurface drainage system decreased soil salinity and lowered the watertable.
Where conditions allow, it will be grown often in areas with a high watertable to allow production in the dry season.
Often, therefore, crops are grown in areas with a high watertable at this time.
On the other hand, no attempts were made (at the policy level) to strengthen the natural resource base in terms of replenishing the watertable.
An optimal tax will differ by location on the aquifer and will change over time as the watertable and demands change.
This would be expected where a subaerial pipe met the watertable.
The alternating dark and light gypsum couplets are attributed to pulsating episodes of the watertable.
Leakage between the nozzle and watertable was prevented by the use of grease and weights.
In wetland habitats, the amplitude of daily fluctuating temperatures becomes large in spring, due to an increasing irradiance and a lowering of the watertable.
These soils generally have a shallow saline watertable and often remain waterlogged or submerged for quite a long time.
The watertable in the dry season was also deeper than in the wet season, resulting in higher percolation losses.
The elevation of the top of the ledge should therefore reflect the height of the watertable.
A large proportion of the households draw water from the shallow watertable.
A capacitance proximity gauze was mounted on a movable gantry spanning the width of the watertable.
The watertable is controlled in the fields by equidistant drains (tertiary canals), which empty into peripheral canals (secondary canals) on which barges navigate.
It is more likely to have been formed by tectonic and solutional activity along a vertical joint entirely below the watertable.
Optimizing water management and nitrogen fertilization under shallow watertable conditions.
This watertable would have settled various sedimentary deposits.
When the watertable was above the soil surface, the depth was measured directly.
Below the watertable soil is almost completely saturated and gasses travel relatively slowly by diffusion through the water.
A high watertable in grassland sites eliminates the possibility of burrowing deep to escape hostile surface conditions.
To avoid increased accession to the watertable, guidelines are in place, setting maximum water use levels depending on irrigation and drainage infrastructure.
Herbaceous vegetation with hygro-halophyllous plant species dominate in lower areas, under fluvial and watertable influences, while halophyllous succulent scrublands are associated with elevated areas occasionally subject to flooding.
At the moment, rainwater seeps away naturally down to the watertable.
Many ecological factors are associated with altitude, including light availability in the understorey, soil texture, leaf-litter t hickness, depth to watertable, and frequency of inundation.
The watertable was of great importance.
By the mid1970s, a falling watertable and declining soil fertility in the longestcultivated village gardens were requiring growers to spend more on fertilisers and motorised pumps.
The impact of the declining watertable and the drying up of open wells is reflected in the changes in the composition of wells over the period.
Tectonics and basin inversion resulted in the collapse of coal measure forests only locally, that is, where they resulted in watertable drop and improved drainage.
These effluents also pose a threat to inland and coastal fisheries and seepage into the watertable means an entry of toxic chemicals into the soil and food chain.
The most important reason, according to the farmers, for the increase in bore wells is the declining watertable and the drying up of open wells (table 7).
One could have a part of a watershed where the watertable was very near the surface.
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As everyone knows, the raising or lowering of the watertable can very often change the plant life on the land.
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Similarly, if there is a borehole used for spray irrigation in a big way, that may lower the watertable all round.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Work is in hand to catch and store water in the upper watertable, and geological surveys are being undertaken to find other underground sources.
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Moreover, the level of the watertable in that area shows no change at all.
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Now that the watertable has fallen and the area is dry, it looks as thought there is a breach in the walls.
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It has been suggested that it will lower the watertable, but how can that be?
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We are well aware of the possible adverse impact on the watertable level that can arise from the poor siting of tube wells.
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I am advised that there is no danger to the public through leaching of sulphide into the watertable.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Restoration is much easier where the working is shallow than where it is below the watertable level.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
When mines close and pumping stops, the watertable rises.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Then drainage or extraction of water by the water companies often changes the levels and the watertable, which in turn affects the foundations.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
The cost of obtaining a potable water supply or stabilising the local watertable have not been investigated.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
The pollution is ultimately seeping through into the watertable.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Nobody can lower the watertable by draining on the other side of a watershed.
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It will drain off into the watertable and our areas have aquifers underneath the clay into which that water will drain.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
At the same time, the watertable is falling in many key agricultural areas.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
What happens where the general watertable falls is that the farm wells do not fill up as quickly as they do normally.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
I accept the point about the high watertable and understand that that can be an effective argument in certain areas.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
However, high watertable levels persist and pumping is continuing.
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And the watertable in those cases where artesian wells are used, continues to fall.
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The second sort of flooding comes from the level of the watertable.
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It defined the cause as being the high level of the watertable.
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The other point is the constant lowering of the watertable.
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The canal has become part of the watertable.
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Underground tests are less of an environmental hazard than atmospheric tests, but underground tests produce radioactivity which seeps into the watertable.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Abstraction of water lowers the watertable and the whole ecology of the area is changed.
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The watertable dropped and the artesian head was destroyed.
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On the environment front, the expectation is that the watertable will be maintained at a reasonably high level.
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Over the years due to corrosion and liberation of the material, the leakage had penetrated as far as a watertable.
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It is difficult to predict to what level the watertable will rebound.
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The raising of the watertable causes flooding in basements and so on and other underground parts of buildings and structures.
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What we need is less abstraction from the watertable.
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We really do have to be sensitive to the dangers to the water supply and to the watertable features.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
The consideration of the conditions would, of course, take into account also such matters as the risk of polluting the underlying watertable.
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
Let us trace the watertable and find out precisely where it is and the movement of the flow.
From the
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Example from the Hansard archive. Contains Parliamentary information licensed under the Open Parliament Licence v3.0
These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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