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estuary    音标拼音: ['ɛstʃu,ɛri]
n. 河口,江口

河口,江口

estuary
n 1: the wide part of a river where it nears the sea; fresh and
salt water mix

Estuary \Es"tu*a*ry\, n.; pl. {Estuaries}. [L. aestuarium, from
aestuare to surge. See {Estuate}.] [Written also
{[ae]stuary}.]
1. A place where water boils up; a spring that wells forth.
[Obs.] --Boyle.
[1913 Webster]

2. A passage, as the mouth of a river or lake, where the tide
meets the current; an arm of the sea; a frith.
[1913 Webster]

it to the sea was often by long and wide estuaries.
--Dana.
[1913 Webster]


Estuary \Es"tu*a*ry\, a.
Belonging to, or formed in, an estuary; as, estuary strata.
--Lyell.
[1913 Webster]


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  • Rivers, Estuaries, Deltas - Woods Hole Oceanographic Institution
    Rivers, estuaries, and deltas are key to understanding the chemical structure of seawater, and are home to some of the world's most diverse ecosystems
  • Brackish Water: Where Fresh Water Rivers Meet A Salt Water Sea
    How does an estuary work? From a physicist’s point of view, the density difference between fresh and salt water makes estuaries interesting When river water meets sea water, the lighter fresh water rises up and over the denser salt water Sea water noses into the estuary beneath the outflowing river water, pushing its way upstream along the bottom Often, as in the Fraser River, this occurs
  • jc006893 1. - Woods Hole Oceanographic Institution
    In the absence of rotational effects, stratification in the estuary decreases following both down-estuary and up-estuary winds, but stratification experiences larger reduction and takes longer to recover under up-estuary winds
  • New perspectives on radium behavior within a subterranean estuary
    Many studies have used the unique geochemical signal originating from the subterranean estuary to determine rates of transport of such cons- tituents to the coastal ocean via submarine groundwater discharge (Burnett et al , 2006 and references therein)
  • Subtidal Salinity and Velocity in the Hudson River Estuary . . .
    A tidally and cross-sectionally averaged model based on the temporal evolution of the quasi-steady Hansen and Rattray equations is applied to simulate the salinity distribution and vertical exchange flow along the Hudson River estuary The model achieves high skill at hindcasting salinity and residual velocity variation during a 110-day period in 2004 covering a wide range of river discharges
  • Episodic and Long-Term Sediment Transport Capacity in The Hudson River . . .
    Abstract A tidally averaged model of estuarine dynamics is used to estimate sediment transport in the Hudson River estuary over the period 1918 to 2005 In long-term and seasonal means, along-channel gradients in sediment flux depend on the estuarine salinity gradient and along-channel depth profile Lateral depth variation across the estuary affects the near-bottom baroclinic circulation and
  • Eglinton, T - Woods Hole Oceanographic Institution
    Walker, S E , Dickhut, R M , Chisholm-Brause, C , Sylva, S , and Reddy, C M , Molecular and isotopic identification of PAH sources in a highly industrialized urban estuary, Organic Geochemistry, 2005; v36, 619-632 Sources of polycyclic arom hydrocarbons (PAHs) in sediments in the Elizabeth River, VA, a highly industrialized urban estuary, were examd using multiple source identification
  • Distribution of anaerobic ammonia-oxidizing bacteria in a subterranean . . .
    The ladderane fatty acid pro le shows three regions of high con-fi centration within the subterranean estuary at depths that correspond to the URTZ, MRTZ, and DRTZ, in addition to high concentration in a surface sample that had a soil-like consistency
  • pH-Dependent iron oxide precipitation in a subterranean estuary
    Here, we implement a simple reaction network in a 1D reactive transport model (RTM), to investigate the effect of O2 and pH gradients along a flow-line in the subterranean estuary of Waquoit Bay (Cape Cod, Massachusetts) on oxidative precipitation of Fe(II) and subsequent PO4 sorption
  • jc005806 1. . 21 - Woods Hole Oceanographic Institution
    1 Introduction [2] Estuarine conditions depend on fluvial, tidal, and baroclinic forcing The river supplies a mean volume flux and a source of buoyancy, tidal oscillations generate currents and a source of turbulent mixing, and the density gradient between fresh and salt water drives baroclinic circulation The relative balance among these factors determines char-acteristics of an estuary





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