n.

流れ、水流、ストリーム

v.

流動する

関: current、flow、flux、mobilization、river、streaming

WordNet

to extend, wave or float outward, as if in the wind; "their manes streamed like stiff black pennants in the wind"
something that resembles a flowing stream in moving continuously; "a stream of people emptied from the terminal"; "the museum had planned carefully for the flow of visitors" (同)flow
exude profusely; "She was streaming with sweat"; "His nose streamed blood"
dominant course (suggestive of running water) of successive events or ideas; "two streams of development run through American history"; "stream of consciousness"; "the flow of thought"; "the current of history" (同)flow, current
a natural body of running water flowing on or under the earth (同)watercourse
flow freely and abundantly; "Tears streamed down her face" (同)well out
cause to flow; "The artist flowed the washes on the paper"
the amount of fluid that flows in a given time (同)flow_rate, rate of flow
any uninterrupted stream or discharge
cover or swamp with water
the act of flowing or streaming; continuous progression (同)stream
the motion characteristic of fluids (liquids or gases) (同)flowing
move or progress freely as if in a stream; "The crowd flowed out of the stadium" (同)flux
be abundantly present; "The champagne flowed at the wedding"
a state of uncertainty about what should be done (usually following some important event) preceding the establishment of a new direction of action; "the flux following the death of the emperor" (同)state of flux
a substance added to molten metals to bond with impurities that can then be readily removed
excessive discharge of liquid from a cavity or organ (as in watery diarrhea)
the rate of flow of energy or particles across a given surface
in constant change; "his opinions are in flux"; "the newness and flux of the computer industry"
a flow or discharge (同)fluxion
occurring in or belonging to the present time; "current events"; "the current topic"; "current negotiations"; "current psychoanalytic theories"; "the ships current position"
a flow of electricity through a conductor; "the current was measured in amperes" (同)electric_current
a steady flow of a fluid (usually from natural causes); "the raft floated downstream on the current"; "he felt a stream of air"; "the hose ejected a stream of water" (同)stream
act of marshaling and organizing and making ready for use or action; "mobilization of the countrys economic resources" (同)mobilisation
act of assembling and putting into readiness for war or other emergency: "mobilization of the troops" (同)mobilisation, militarization, militarisation
a large natural stream of water (larger than a creek); "the river was navigable for 50 miles"
exuding a bodily fluid in profuse amounts; "his streaming face"; "her streaming eyes"
(computer science) using or relating to a form of continuous tape transport; used mainly to provide backup storage of unedited data; "streaming audio"; "streaming video recording"

PrepTutorEJDIC

『小川』,流れ / (気体・液体の)『流れ』《+of+名》 / (人・車などの)連続した動き,流れ《+of+名》・《単数形で》世論の動向,風潮;(思考などの)流れ《+of+名》・〈液体が〉『流れる』・(を)流し出す,流す《+with+名》・〈人などが〉流れるように続く,絶えず続く・〈旗などが〉ひるがえる,なびく・〈液体〉‘を'流し出す,流す
《副詞巳句始を伴って》〈気体・液体・電気などが〉『流れる』 / 《副詞[句]を伴って》〈言葉・人々などず〉流れるように続く / 〈心・場所などが〉(…で)いっぱいになる,満ちあふれる《+『with』+『名』》 / 《副詞[句]を伴って》〈髪・服などが〉長く垂れる;風になびく / 〈潮が〉満ちる / (…から)生じる,発生する《+『from』+『名』》 / 〈C〉《単数形で》(気体・液体・電気などの)『流れ』《+『of』+『名』》 / 〈C〉《単数形で》(言葉・人などの)絶え間のない(よどみのない)流れ《+『of』+『名』》 / 〈C〉《単数形で》(…の)洪水,はんらん《+『of』+『名』》 / 〈U〉《the flow》満ち潮,上げ潮
流動,流れ;上げ潮 / 絶え間ない変化,流転(るてん) / 融剤,フラックス / (流体・粒子・エネルギーの)流量,流束,流動率 / (電気・磁気の)束(そく) / (体内の液体の)異常流出,異常排出
『通用している』,流通している,一般に行われている / 『今の』,『現在の』 / 〈C〉(水・空気などの)『流れ』,流動 / 〈C〉〈U〉電流 / 〈C〉(…の)『流れ』,『風潮』,動向《+『of』+『名』》
『川』 / (水以外のものの)流れ,多量の流出《+『of』+『名』》

Wikipedia preview

出典(authority):フリー百科事典『ウィキペディア（Wikipedia）』「2015/08/19 11:28:04」(JST)

A stream is a body of water^[1] with a current, confined within a bed and stream banks. Depending on its location or certain characteristics, a stream may be referred to as a branch, brook, beck, burn, creek, crick, gill (occasionally ghyll), kill, lick, mill race, rill, river, syke, bayou, rivulet, streamage, wash, run, or runnel.

Streams are important as conduits in the water cycle, instruments in groundwater recharge, and corridors for fish and wildlife migration. The biological habitat in the immediate vicinity of a stream is called a riparian zone. Given the status of the ongoing Holocene extinction, streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity. The study of streams and waterways in general is known as surface hydrology and is a core element of environmental geography.^[2]

Types

Stream in Arkhangelsk Oblast, Russia

A rocky creek in Spearfish Canyon, US

Creek in Australia

Wyming Brook in Sheffield, UK

Brook in the Bay of Fundy, Canada

A low level stream in Macon County, Illinois

Brook: A stream smaller than a creek, especially one that is fed by a spring or seep. It is usually small and easily forded. A brook is characterised by its shallowness and its bed being composed primarily of rocks.
Creek

In North America, Australia and New Zealand, a small to medium-sized natural stream. Sometimes navigable by motor craft and may be intermittent.
In parts of New England,^[3] the UK and India, a tidal inlet, typically in a salt marsh or mangrove swamp, or between enclosed and drained former salt marshes or swamps (e.g. Port Creek separating Portsea Island from the mainland). In these cases, the stream is the tidal stream, the course of the seawater through the creek channel at low and high tide.

River: A large natural stream, which may be a waterway.
Runnel: the linear channel between the parallel ridges or bars on a shoreline beach or river floodplain, or between a bar and the shore. Also called a swale.
Tributary: A contributory stream, or a stream which does not reach the sea but joins another river (a parent river). Sometimes also called a branch or fork.

Other names

In the United Kingdom, there are several regional names for a stream:

Allt is used in Highland Scotland.
Beck is used in Yorkshire, Lancashire, Dumfriesshire, Cumbria, Norfolk, and Lincolnshire.
Bourne is used in the chalk downland of southern England (although strictly a bourne is wet in summer and dry in winter).
Brook is used in the Midlands, Lancashire and Cheshire.
Burn is used in Scotland and North East England.
Nant is used in Wales.
Rivulet is an term encountered in Victorian era publications.
Stream is used in Southern England.
Syke is used in lowland Scotland and Cumbria for a seasonal stream.

In North America:

Branch, fork, or prong can refer to tributaries or distributaries that share the same name as the main stream, generally with the addition of a cardinal direction.
Branch is also used to name streams in Maryland and Virginia.
Crick is used in some parts of the United States.
Falls is also used to name streams in Maryland. Little Gunpowder Falls and The Jones Falls are actually rivers named in this manner, unique to Maryland.
Kill in New York, Pennsylvania, Delaware, and New Jersey comes from a Dutch language word meaning "riverbed" or "water channel", and can also be used for the UK meaning of 'creek'.
Run in Ohio, Maryland, Michigan, Pennsylvania or Virginia can be the name of a stream.
Run in Florida, is the name given to streams coming out of small natural springs. River is used for larger springs like the Silver River and Rainbow River.
Stream and brook are used in Midwestern states, Mid-Atlantic states, and New England.

Bar: A shoal that develops in a stream as sediment is deposited as the current slows or is impeded by wave action at the confluence.
Bifurcation: A fork into two or more streams.
Channel: A depression created by constant erosion that carries the stream's flow.
Confluence: The point at which the two streams merge. If the two tributaries are of approximately equal size, the confluence may be called a fork.
Floodplain: Lands adjacent to the stream that are subject to flooding when a stream overflows its banks.
Gauging station: A point of demarcation along the route of a stream or river, used for reference marking or water monitoring.
Headwaters: The part of a stream or river proximate to its source. The word is most commonly used in the plural where there is no single point source.
Knickpoint: The point on a stream's profile where a sudden change in stream gradient occurs.
Mouth: The point at which the stream discharges, possibly via an estuary or delta, into a static body of water such as a lake or ocean.
Pool: A segment where the water is deeper and slower moving.
Riffle: A segment where the flow is shallower and more turbulent.
River: A large natural stream, which may be a waterway.
Run: A somewhat smoothly flowing segment of the stream.
Source: The spring from which the stream originates, or other point of origin of a stream.
Spring: The point at which a stream emerges from an underground course through unconsolidated sediments or through caves. A stream can, especially with caves, flow aboveground for part of its course, and underground for part of its course.
Stream bed: The bottom of a stream.
Stream corridor: Steam, its floodplains, and the transitional upland fringe^[4]
Thalweg: The river's longitudinal section, or the line joining the deepest point in the channel at each stage from source to mouth.
Waterfall or cascade: The fall of water where the stream goes over a sudden drop called a nickpoint; some nickpoints are formed by erosion when water flows over an especially resistant stratum, followed by one less so. The stream expends kinetic energy in "trying" to eliminate the nickpoint.
Wetted perimeter: The line on which the stream's surface meets the channel walls.

Sources

Small tributary stream, Diamond Ridge, Alaska

Creek in Perisher Ski Resort, Australia

Streams typically derive most of their water from precipitation in the form of rain and snow. Most of this water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants. Some of the water proceeds to sink into the earth by infiltration and becomes groundwater, much of which eventually enters streams. Some precipitated water is temporarily locked up in snow fields and glaciers, to be released later by evaporation or melting. The rest of the water flows off the land as runoff, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth. Some creeks may start from ponds or lakes.

Characteristics

Ranking

To qualify as a stream it must be either recurring or perennial. Recurring (intermittent) streams have water in the channel for at least part of the year. A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. Thus, if a first-order stream joins a second-order stream, it remains a second-order stream. It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream.

Gradient

The gradient of a stream is a critical factor in determining its character and is entirely determined by its base level of erosion. The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream.

In geological terms, the stream will erode down through its bed to achieve the base level of erosion throughout its course. If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander.

Meander

Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine in form. Typically, over time the meanders gradually migrate downstream.

If some resistant material slows or stops the downstream movement of a meander, a stream may erode through the neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou. A flood may also cause a meander to be cut through in this way.

Profile

Typically, streams are said to have a particular profile, beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream. However, a stream may meander for some distance before falling into a "young" stream condition.

Stream load

Streams can carry sediment, or alluvium. The amount of load it can carry (capacity) as well as the largest object it can carry (competence) are both dependent on the velocity of the stream.

Intermittent and ephemeral streams

Australian creek, low in the dry season, carrying little water. The energetic flow of the stream had, in flood, moved finer sediment further downstream. There is a pool to lower right and a riffle to upper left of the photograph.

A perennial stream is one which flows continuously all year.^[5]^:57 Some perennial streams may only have continuous flow in segments of its stream bed year round during years of normal rainfall.^[6]^[7]

Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line.

Intermittent stream

In the United States, an intermittent or seasonal stream is one that only flows for part of the year and is marked on topographic maps with a line of blue dashes and dots.^[5]^:57–58 A wash or desert wash is normally a dry streambed in the deserts of the American Southwest which flows only after significant rainfall. Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions. These flash floods often catch travelers by surprise. An intermittent stream can also be called an arroyo in Latin America, a winterbourne in Britain, or a wadi in the Arabic-speaking world.

In Italy an intermittent stream is termed a torrent (Italian torrente). In full flood the stream may or may not be "torrential" in the dramatic sense of the word, but there will be one or more seasons in which the flow is reduced to a trickle or less. Typically torrents have Apennine rather than Alpine sources, and in the summer they are fed by little precipitation and no melting snow. In this case the maximum discharge will be during the spring and autumn. However, there are also glacial torrents with a different seasonal regime.

In Australia, an intermittent stream is usually called a creek and marked on topographic maps with a solid blue line.

Ephemeral stream

Generally, streams that flow only during and immediately after precipitation are termed ephemeral. There is no clear demarcation between surface runoff and an ephemeral stream.^[5]^:58

Drainage basins

The extent of land basin drained by a stream is termed its drainage basin (also known in North America as the watershed and, in British English, as a catchment).^[8] A basin may also be composed of smaller basins. For instance, the Continental Divide in North America divides the mainly easterly-draining Atlantic Ocean and Arctic Ocean basins from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (This delineation is termed the Eastern Continental Divide.) Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as the Tombigbee River basin. Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth.

References

^ Langbein, W.B.; Iseri, Kathleen T. (1995). "Hydrologic Definitions: Stream". Manual of Hydrology: Part 1. General Surface-Water Techniques (Water Supply Paper 1541-A). Reston, VA: USGS. .
^ U.S. Geological Survey (USGS). Atlanta, GA. "What is hydrology and what do hydrologists do?" 2009-05-13.
^ Spruce Creek Association. Kittery, ME. "About the Spruce Creek Watershed." Accessed 2010-10-02.
^ "Stream Corridor Structure" Adapted from Stream Corridor Restoration: Principles, Processes, and Practices
^ ^a ^b ^c Meinzer, Oscar E. (1923). Outline of ground-water hydrology, with definitions. Washington, DC: USGS. Water Supply Paper 494.
^ Meinzer, Oscar E. (1923). Outline of ground-water hydrology, with definitions. Washington, DC: US Geological Survey (USGS). p. 57. Water Supply Paper 494.
^ "OSM - COALEX State Inquiry Report 97". Retrieved 2011-12-11.
^ Langbein, W.B.; Iseri, Kathleen T. (1995). "Hydrologic Definitions: Watershed". Manual of Hydrology: Part 1. General Surface-Water Techniques (Water Supply Paper 1541-A). Reston, VA: USGS.

External links

Glossary of stream-related terms, StreamNet

UpToDate Contents

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English Journal

Elements of concern in fillets of bighead and silver carp from the Illinois River, Illinois.

Levengood JM1, Soucek DJ2, Sass GG2, Dickinson A2, Epifanio JM2.Author information 1Illinois Natural History Survey, University of Illinois at Urbana-Champaign, 1816 S. Oak St., Champaign, IL 61820, United States. Electronic address: levengoo@illinois.edu.2Illinois Natural History Survey, University of Illinois at Urbana-Champaign, 1816 S. Oak St., Champaign, IL 61820, United States.AbstractEfforts to control invasive bighead (Hypophthalmichthys nobilis) and silver carp (H. molitrix) may include harvest for human consumption. We measured concentrations of arsenic (As), mercury (Hg), and selenium (Se) in fillets from silver and bighead carp collected from the lower Illinois River, Illinois, USA, to determine whether concentrations were of health concern and differed by species, size, and location. Concentrations of total As were below detection limits in most bighead (92%) and silver (77%) carp fillets, whereas inorganic As was below detection limits in all samples. Mean Hg concentrations were greater in bighead (0.068mgkg(-1)) than in silver carp (0.035mgkg(-1)), and were smallest in carp from the confluence of the Illinois and Mississippi rivers. Mercury concentrations in fillets were positively correlated with body mass in both species. Concentrations of Hg were below the US Food and Drug Administration's (USFDA) action level (1ppm as methyl-Hg); however, concentrations in some bighead (70%) and silver (12%) carp fell within the range that would invoke a recommendation to limit meals in sensitive cohorts. Mean Se concentrations were greater in silver (0.332mgkg(-1)) than in bighead (0.281mgkg(-1)) carp fillets, and were below the 1.5mgkg(-1) limit for an unrestricted number of meals/month. The mean molar ratio of Se:Hg in fillets was lower in bighead (14.0) than in silver (29.1) carp and was negatively correlated with mass in both species Concentrations of Hg in bighead and silver carp fillets should be considered when assessing the risks associated with the use of these species as a protein source.
Chemosphere.Chemosphere.2014 Jun;104:63-8. doi: 10.1016/j.chemosphere.2013.10.058. Epub 2013 Dec 2.
Efforts to control invasive bighead (Hypophthalmichthys nobilis) and silver carp (H. molitrix) may include harvest for human consumption. We measured concentrations of arsenic (As), mercury (Hg), and selenium (Se) in fillets from silver and bighead carp collected from the lower Illinois River, Illin
PMID 24300421

Stable water isotope patterns in a climate change hotspot: the isotope hydrology framework of Corsica (western Mediterranean).

van Geldern R1, Kuhlemann J, Schiebel R, Taubald H, Barth JA.Author information 1a GeoZentrum Nordbayern, Department of Geography and Geosciences , Friedrich-Alexander-University Erlangen-Nuremberg , Erlangen , Germany.AbstractThe Mediterranean is regarded as a region of intense climate change. To better understand future climate change, this area has been the target of several palaeoclimate studies which also studied stable isotope proxies that are directly linked to the stable isotope composition of water, such as tree rings, tooth enamel or speleothems. For such work, it is also essential to establish an isotope hydrology framework of the region of interest. Surface waters from streams and lakes as well as groundwater from springs on the island of Corsica were sampled between 2003 and 2009 for their oxygen and hydrogen isotope compositions. Isotope values from lake waters were enriched in heavier isotopes and define a local evaporation line (LEL). On the other hand, stream and spring waters reflect the isotope composition of local precipitation in the catchment. The intersection of the LEL and the linear fit of the spring and stream waters reflect the mean isotope composition of the annual precipitation (δP) with values of-8.6(±0.2) ‰ for δ(18)O and-58(±2) ‰ for δ(2)H. This value is also a good indicator of the average isotope composition of the local groundwater in the island. Surface water samples reflect the altitude isotope effect with a value of-0.17(±0.02) ‰ per 100 m elevation for oxygen isotopes. At Vizzavona Pass in central Corsica, water samples from two catchments within a lateral distance of only a few hundred metres showed unexpected but systematic differences in their stable isotope composition. At this specific location, the direction of exposure seems to be an important factor. The differences were likely caused by isotopic enrichment during recharge in warm weather conditions in south-exposed valley flanks compared to the opposite, north-exposed valley flanks.
Isotopes in environmental and health studies.Isotopes Environ Health Stud.2014 Jun;50(2):184-200. doi: 10.1080/10256016.2013.839559. Epub 2014 Jan 20.
The Mediterranean is regarded as a region of intense climate change. To better understand future climate change, this area has been the target of several palaeoclimate studies which also studied stable isotope proxies that are directly linked to the stable isotope composition of water, such as tree
PMID 24437609

Motives for meaningful involvement in rural AIDS service organizations.

Paterson BL1, Ross S, Gaudet T.Author information 1a School of Nursing , Thompson Rivers University , British Columbia , V2C 5N3 , Canada.AbstractThe research described herein was a three-year exploratory descriptive study to examine how meaningful involvement (MIPA) is conceptualized and experienced in rural regions of the Maritime provinces of Canada. The focus of this paper is one aspect of the research; i.e., what motivates the clients of AIDS Service Organizations (ASOs) in rural Canada to become meaningfully involved? We interviewed 34 people who were past or current clients of ASOs in Maritime Canada and who self-reported as engaging in at-risk behaviors for HIV or living with HIV. The interviews explored participants' perspectives about their motives for becoming meaningfully involved in an ASO. Three themes regarding motives for MIPA were revealed: (1) meeting personal needs; (2) making a difference to others; and (3) recognizing a fit between their skills, goals, needs and the opportunities and experiences within the ASO and with other ASO clients. Participants generally cited more than one motive. This research study contributed to the field of knowledge about the motives for MIPA in which it reveals (1) that MIPA was conceptualized by the rural ASO clients as whatever participation provided them personal meaning (i.e., by fulfilling a personal need, by making a difference, and by recognizing a fit) and (2) the important role that ASO staff and volunteers have in fostering and sustaining MIPA. The study also highlighted a trajectory of involvements that support the need for ASOs to entertain a wide range of roles that are assumed as MIPA.
AIDS care.AIDS Care.2014 May;26(5):582-6. doi: 10.1080/09540121.2013.843771. Epub 2013 Oct 10.
The research described herein was a three-year exploratory descriptive study to examine how meaningful involvement (MIPA) is conceptualized and experienced in rural regions of the Maritime provinces of Canada. The focus of this paper is one aspect of the research; i.e., what motivates the clients of
PMID 24111835

Reconstructing long-term trends in municipal sewage discharge into a small lake in northern Manitoba, Canada.

Tse TJ1, Codling G2, Jones PD3, Thoms K4, Liber K2, Giesy JP5, Wheater H6, Doig LE7.Author information 1Toxicology Graduate Program, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B3, Canada.2Toxicology Center, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B3, Canada.3Toxicology Center, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B3, Canada; School of Environment and Sustainability, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5C3, Canada.4Saskatchewan Structural Sciences Centre, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5C9, Canada.5Toxicology Center, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B3, Canada; Department of Veterinary Biomedical Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B4, Canada.6Global Institute for Water Security, University of Saskatchewan, Saskatoon, Saskatchewan S7N 3H5, Canada.7Toxicology Center, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5B3, Canada. Electronic address: lorne.doig@usask.ca.AbstractRoss Lake lies within the City of Flin Flon (Manitoba, Canada), a mining community originally formed by the Hudson Bay Mining and Smelting Company (now Hudbay Minerals Inc.) in 1927. At the time of this investigation, a continuous effluent stream from Hudbay Minerals (approximately 80years) and a discontinuous and unknown amount of raw and minimally treated municipal sewage (>20years, likely ending in 1951) was discharged into the north basin of the lake. Maximum concentrations of fecal sterols, such as coprostanol and terrestrial phytosterols, such as: β-sitosterol, campesterol, stigmastanol were measured in vertical sections of sediment cores, collected from Ross Lake, in the 15-16-cm section, which likely corresponds to the 1930s. Concentrations of coprostanol increased from <1μgg(-1) in older sediments, to 252.3μgg(-1) organic carbon at the peak. Observed changes in concentrations of sterols, in combination with radiometric dating and changes to sediment physicochemical characteristics, support the conclusion that sediments of a depth of less than 17.5-cm depth were deposited during the post-industrial era from approximately 1930 onwards. Ratios of coprostanol to cholesterol >1, peaking at 3.6 are consistent with anecdotal information that municipal sewage was discharged into Ross Lake during the early years of urbanization, prior to changes in treatment of sewage and discharge practices that began in 1951. Finally, historical concentrations of terrestrial phytosterols followed trends similar to those of coprostanol and cholesterol and may possibly be the result of an increase in the flux of terrestrial organic matter into Ross Lake as the result of regional deforestation due to logging and fire.
Chemosphere.Chemosphere.2014 May;103:299-305. doi: 10.1016/j.chemosphere.2013.12.019. Epub 2014 Jan 7.
Ross Lake lies within the City of Flin Flon (Manitoba, Canada), a mining community originally formed by the Hudson Bay Mining and Smelting Company (now Hudbay Minerals Inc.) in 1927. At the time of this investigation, a continuous effluent stream from Hudbay Minerals (approximately 80years) and a di
PMID 24405965

Japanese Journal

クリエイティブナビ COMMERCIAL FILM NEWSPAPER/GRAPHIC WEB/STREAM

ブレーン = Brain 55(5), 141-155, 2015-05
NAID 40020417605

ASIA STREAM 朝鮮半島 2015年2~3月三年ぶりの日中韓外相会議と続く不協和音

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東亜 (574), 78-86, 2015-04
NAID 40020415418

ASIA STREAM 台湾 2015年2~3月不穏な空気が流れる総統、国民党主席、立法院長の関係

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東亜 (574), 66-76, 2015-04
NAID 40020415411

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NAID 40020415406

Related Pictures

★リンクテーブル★

リンク元	「流動」「flow」「current」「flux」「流れ」
拡張検索	「catheter related blood stream infection」「upstream promotor element」
関連記事	「streaming」