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Weblio 辞書 > 英和辞典・和英辞典 > sedimentの意味・解説 > sedimentに関連した共起表現

「sediment」の共起表現一覧(1語右で並び替え)

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Because it is in an area of active sediment accumulation by rivers, it must be a geologic
Parameters to measure are sediment accumulation, turbidity at the level of the f
ving center channel which reduces the rate of sediment accumulation, while slowing water flow near t
ion on the outside of the meander, and sweeps sediment across the floor of the meander towards the i
For deposits of sediment across the earth's surface, see Chevron (land
he plant season by season, and changes in the sediment amounts entering the habitat by water flow.
Explosively evert pharynx into sediment, anchor position with prostomium and pull bod
w) brings up samples of seawater, ocean floor sediment, and plankton.
tle University, after the introduction of the sediment and solute transport component.
ock's access to the stream, which will reduce sediment and contamination from fecal bacteria, and pl
t-water interface is the boundary between bed sediment and the overlying water column.
6m grids where two teams began excavating the sediment and recovering the small finds, once a grid w
ired Waters for fecal, metal, toxic chemical, sediment, and nutrients.
and bridges, and washing thousands of tons of sediment and wreckage into San Diego Bay.
a grass channel or swale, in order to capture sediment and avoid clogging the trench.
ters are most effective at removing chlorine, sediment, and volatile organic compounds (VOCs) from w
ic and chemical characteristics of the bottom sediment and the aquifer, the local recharge-discharge
The accumulation of sediment and deposits on heat transfer surfaces in coo
Landslides occurred in unconsolidated sediment and fissures up to 30 cm wide were observed.
ict the erosion, transport, and deposition of sediment and solutes in landscapes and sedimentary bas
o define a concentration profile of suspended sediment and which also determines how sediment will b
hristchurch Bay, it transported and deposited sediment and shingle onto what is now known as Hurst C
er of equipment for the automated analysis of sediment and rock cores.
ow covered by countless thousands of years of sediment and glacial deposits.
It is cloudy, has a sediment and is quite dry, this is very different from
ect the portions of the falls covered over by sediment and therefore temporarily immune to direct we
Thick layers of sediment and carbonate rock were deposited on the shal
nder water as a small brown ring in soft fine sediment and slightly submerged.
idely distributed in soil, hot springs, ocean sediment, and is a cause of spoilage in food products.
It represents the remains of fluvio-deltaic sediment, and consists mainly of clastic rocks (clayst
used by an object that was dug into the muddy sediment and then lifted out.
Major contaminants in the soil, sediment, and groundwater are volatile organic compoun
with the pointed end of the cone down in the sediment and the broad end upwards.
of a lithified rock and becoming a brand new sediment and rock.
and 2005, Wax Lake was completely filled with sediment, and the delta prograded approximately 8 km i
which the bed and banks are made up of mobile sediment and/or soil.
thod by which successive layers of basin fill sediment are "stripped off" the total stratigraphy dur
tals by direct chemical analysis in water and sediment are limited in reliability.
nerally a suspension feeder normally found on sediment areas.
The land is formed from sediment at the mouth of the Guadalquivir river.
of the liquid in the coffee is drunk, but the sediment at the bottom is left behind.
sted to leave a small amount of the beer with sediment at the bottom of the bottle, then swirl it ar
owries live in cold deep waters on the bottom sediment at about 100-200 metres (330-660 ft) of depth
BBL) is the layer of water directly above the sediment at the bottom of a river, lake or sea.
barrels built up a deposit of strongly sweet sediment at the bottom, which was melted out with boil
llowed the uninterrupted build-up of 400 m of sediment at the bottom of the lake, recording informat
olluted in Minnesota, with elevated levels of sediment, bacteria, nitrates, phosphorus, mercury, PCB
Sediment basin
rial mass flows happen when a large amount of sediment becomes unstable, this can happen for example
gs that reveal regional unconformities in the sediment bed of Long Island Sound.
e created erosion problems, leading to excess sediment being transported downstream into the River,
nt tsunami have been recorded, with deposited sediment being discovered in Montrose Basin, the Firth
versity found two distinct layers of sand and sediment between the clay deposited on the river bank
unnel passes on a 300 metre causeway over the sediment bowl of the latter plant.
f a borehole by examining the bits of rock or sediment brought to the surface by the circulating dri
e first is river delta alluvial deposition of sediment brought in by the rivers which flow into the
n (sludging is digging or sifting through the sediment build up of municipal storm drains and old se
enecks, predicting local flooding, estimating sediment build-up and transport, optimization and desi
ollowing year the Sakawa River flooded due to sediment build-up resulting from the ash fall, and the
the dam for power generation until 1972, when sediment buildup in Davy Crockett Lake made continued
have increased erosion, leading to excessive sediment buildup in the river and its tributaries.
ves, they are adapted for burrowing into soft sediment, but they are relatively sedentary, rarely mo
ng that the reservoir would have been full of sediment by 2030.
of repichnia caused by disturbances to a soft sediment by a swimming organism, e.g. a benthic fish.
iding, it has been shown that water-saturated sediment can also play up to 90% of the basal movement
The traction caused by this sediment can halt a steadily moving glacier if it inte
; co-discoverer Beauvilain cautions that such sediment can be easily moved by the wind, unlike packe
h a bridge, and to modify the dam so that the sediment can once again be driven out to sea.
river mouth delta is formed by deposition of sediment carried by the stream as the river current di
ormed in the estuary from the large amount of sediment carried in by the Betsiboka River and have be
s, wind-blown dust, grinding by glaciers, and sediment carried by icebergs.
lled the continental rise, which is caused by sediment cascading down the continental slope.
ach, where the borough of Singen has set up a sediment catching facility, catiching sediments and gr
rochemistry, earth and geochemistry, soil and sediment chemistry and chemical toxicology.
abundance of fine-grained sand, but not much sediment coarser, 2) lack of sequence boundaries that
natural gas, mainly methane within a water or sediment column.
horro Creek watershed to reduce the amount of sediment coming into the bay to form bottom layers of
Chemical treatment of sediment, commonly called an active treatment system,
Due to the high sediment concentration in the water, the transfer from
A maximum daily mean of sediment concentration of 41,7000 mg/L was recorded on
e parameter in the Rouse Profile of suspended sediment concentration with depth in a flowing fluid.
gina, the beverage contains a small amount of sediment consisting of grapefruit juice pulp.
tern United States and has increased the high sediment content of the river.
he acidic water, and fine, light-colored ashy sediment continually stirred up by boiling areas.
lower side is the land inned earlier, because sediment continued to build up on the side that remain
her types of erosion models is the use of the sediment continuity equation discussed below.
r Americano Creek released 4,000 tons/year of sediment, contributing to flooding in downstream commu
, field borders, and constructing a water and sediment control basin.
Erosion and sediment control - During excavation of sites, Mammoth
mplement new authority for a soil erosion and sediment control program in this basin that had been e
The Great Lakes Basin Soil Erosion and Sediment Control Program was authorized by the 2002 fa
Chemical sediment control is currently used on some constructio
A silt fence, a type of sediment control, installed on a construction site
l water supplies, stream-pollution abatement, sediment control, preservation and enhancement of fish
morial project teams are tracking erosion and sediment control, stormwater management, and light pol
e, the State of Maryland requires erosion and sediment controls on construction sites of 5,000 sq ft
l sites and their elevated charcoal levels in sediment cores suggest that extensive anthropogenic fo
number of primary sources, including deep-sea sediment cores (and the fossils of phytoplankton and z
limate change, the national archive of subsea sediment cores (BOSCORF), the National Oceanographic L
Moreover, geochemical analysis of sediment cores has allowed for the reconstruction of t
nown from both the fossil record and deep sea sediment cores.
Hodell's research areas include: lake sediment cores; speleothems; marine sediment cores; an
rivers, Lake Powell is gradually filling with sediment, decreasing its capacity; eventually the sedi
agement Tool) - to predict the probability of sediment delivery with various mitigation treatments i
ent and deposition at points along the slope, sediment delivery, and vegetation growth.
The initial porosity of a sediment depends on its lithology.
rosion and redeposited in a currently forming sediment deposit.
ton Delta is a 300-mile-wide clastic wedge of sediment deposited over what is now eastern North Amer
This was originally an island of sand and sediment deposited in the Missouri River by the Boyer
Sediment deposited by glaciers in moraines is characte
arbon dating of plant material recovered from sediment deposited by the tsunami, the latest incident
esponds to small changes in the nature of the sediment deposited.
The year 1938 saw major flooding and sediment deposition along the river.
Two phases of fan sediment deposition were separated by a long period of
m of the delta attests to the balance between sediment deposition by the Ebro and removal of this ma
e able to see their "growth rings" (layers of sediment deposition) and fossilized shells, leaves or
d at the bend of a large river during time of sediment deposition.
ecrease in phosphorus, and a 35% reduction in sediment, despite urban areas increasing to 31% of the
sediment), dissolved chemical species (i.e.
Little Missouri carries heavy loads of eroded sediment downstream.
basin was filled with 400,000 cubic metres of sediment dredged from the Tyne.
sheet pile and have the contaminated muds and sediment dredged and pumped into a disused treatment p
ollowing the alleged illegal dumping of toxic sediment during the development of Falmouth Marina.
gh specific gravity sink to the bottom of the sediment during agitation and remain within the pan fo
nographic circulation studies, including fine sediment dynamics, sea ice simulations, lak hydrodynam
ble for being one of the few areas of Permian sediment east of the Mississippi River.
vere, since due to dams, river regulation and sediment extraction it has lost most of its former hab
Since impact, sediment filled part of the crater, giving it its pres
l sandstone cliffs and interrupts the natural sediment flow of the area.
Fluids such as wind and water, as well as sediment flowing via gravity, transport previously ero
isiana that was formed by rapid deposition of sediment following the creation of a canal through Wax
silisable burrow forms as they penetrated the sediment for protection or to feed.
y a burrowing arthropod ploughing through the sediment for food, leaving a mound of piled sediment a
er gradients where there is a large supply of sediment for braid bars, while single thread sinous ch
the animal (probably a nematode) scoured the sediment for food.
re formed through the gradual accumulation of sediment: for example, sand on a beach or mud on a riv
actions, due to the large amount of trash and sediment found in it.
ebris and oil) and settleable particles, like sediment, from stormwater.
The continuous deposition of sediment from the river and travertine deposits from t
Too much sediment from the stream, some of it from the Woodrow
ce a suitable placer deposit is located, some sediment from it is scooped into a pan, where it is th
After settling the sediment from the received flow, clear water discharge
settling of particles (atoms or molecules) or sediment from a solution, suspension and mixture or va
changers and chillers: Deposits are typically sediment from impurities in the water circulating thro
port of Skagway and, by smaller boat (due to sediment from the Taiya River), the now-ghost town of
Deposition can also refer to the buildup of sediment from organically derived matter or chemical p
of natural fertilizers such as rice straw or sediment from river flooding, and so on.
ntrol the annual flooding, as well as to keep sediment from the flats out of the Chesapeake Bay.
season and washes down an enormous amount of sediment from the mountains producing muds and soils t
hes control surface water runoff, and prevent sediment from escaping the site.
phenomena, mainly from tectonic movement, and sediment from various sources.
A dredge will remove woody sediment from the dam's inside face and, when breached
the area was a river estuary receiving river sediment from land to the west.
rior positioning may be useful for preventing sediment getting into the mantle cavity, which is more
apacity as roughly 1.5 million cubic yards of sediment has filled it in.
an environmental effect on the fjord, and its sediment has become polluted with PCB and mercury.
thick group of volcaniclastic and bentonitic sediment horizons.
The loss of this sediment, however, gives the water extra energy and it
This organism was isolated from sediment in a tropical tank at the Seattle Aquarium by
Transport of sediment in a channel
Average sediment in mouth per year is 113 mm.
d on a train (the movement would shake up the sediment in the barrel and result in an undrinkable pi
Average sediment in mouth per year is 112 mm.
Average sediment in mouth per year is 71 mm.
Average sediment in mouth per year is 129 mm.
Average sediment in mouth per year is 80 mm.
Average sediment in mouth per year is 146 mm.
Average sediment in mouth per year reach 100 mm.
Average sediment in mouth per year is 127 mm.
Average sediment in mouth per year is 92 mm.
For the body of sediment in a river, see Bar (river morphology).
likely caused by the natural flow of silt and sediment in the basin.
The sediment in the bottom of a glass or bottle of wine is
Muddy streams generally have more sediment in the water, reducing clarity.
Her work analysing pollen taken from the sediment in bogs revealed the past botanical assemblag
Silt ( sediment) in runoff from construction sites, logging,
Bed load sediment in the thalweg of Campbell creek in Alaska.
into bedrock by a combination of abrasion as sediment in the flow collides with the channel bed and
causing a severe scouring of the contaminated sediment in the reservoir bed and caused a fish kill d
the wreck was already being covered by fresh sediment in 1981.
an important analogue to craters filled with sediment in a similar way on Mars.
ke in form, adapted for burrowing through the sediment in a fashion similar to earthworms.
do not feed and they spawn close to the soft sediment in which they were previously resident.
The sediment in the submerged river beds from that period
d depressions that filled up with continental sediment in the Tertiary period.
Unless they form a stable bottom sediment in the final container, the spent finings are
g gamma radiation to characterize the rock or sediment in a borehole.
ic failure and subsequent evolution following sediment inhibition and a great storm in October 1996
esent an unusually high supply of terrigenous sediment into the shallow carbonate platform that was
ts of tectonic uplift in nearby areas feeding sediment into the area.
ps wash down an astonishing 2 billion tons of sediment into the plains of India, making it the most
ted as part of a braided river system feeding sediment into the Weald Basin.
Since the sediment is more permeable than the surrounding materi
When a layer of sediment is originally deposited, it contains an open
nd therefore its competence (ability to carry sediment) is increased.
ws merge in a small settling reservoir, where sediment is naturally deposited, and then pumped for t
However, the source of the sediment is termed its provenance.
s routed around the incipient bar, additional sediment is deposited on the incipient bar.
, entrainment is the process by which surface sediment is incorporated into a fluid flow (such as ai
As the sediment is buried it is compacted as more and more ma
                                                                                                    


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