How to use in-sentence of “seawater”:
– It depends on how much seawater flows into it from the Red and the Mediterranean seas.
– In the northeast Pacific Ocean from 0-500m, Nickel concentrations range from 5.54 nmol/kg of seawater to 6.63 nmol/kg of seawater, as there is a region of productivity there.
– This prevents the water in the brine pool from mixing with the ‘normal’ seawater above.
– Chlorine is reacted with seawater to change the iodide to iodine.
– Primary producing prokaryotic communities of brine, interface and seawater above the halocline of deep anoxic lake L’Atalante, Eastern Mediterranean Sea.
– Salt that is gained through evaportation of seawater needs to be cleaned; this is done by dissloving it in brine and then forcing it to crystallize.
– Temporal variations of V in seawater could be controlled by the aforementioned isotope fractionation and fluxes of various V sources and sinks to the ocean that is likely related to the global redox state of the oceans.
– This halocline between the seawater above and the brine below has many bacterial and archaeal cells: they are chemoautotrophs, which feed on ammonia from the brine but cannot function without some oxygen.
Example sentences of “seawater”:
– There they made salt from the seawater and broke a law of British India prohibiting making salt without paying taxes, so this event is referred to as the Salt March.
– Usually, marine light-emission belongs in the blue and green light spectrum, the wavelengths that can transmit through seawater most easily.
– A possible mechanism for the V isotopic offset between seawater and hydrogenous Fe-Mn crusts and nodules is the fractionation during the adsorption of V on the surface of the Fe-Mn oxyhydroxide.
– These are the presence of seawater and the presence of enough light for photosynthesis.
– Vanadium is an element that is widely distributed in Earth’s crust as well as in seawater and groundwater reservoirs.
– The fad for bathing in seawater as a cure for illnesses was encouraged.Seldon, Anthony 2002.
– Changes in local redox conditions impart a significant isotopic fractionation from seawater as recorded in the local sedimentary V isotopic signature.
– The budget of dissolved vanadium in the oceans is remarkably well balanced, with about 40×10 g V/y inputs and outputs, and a mean residence time for dissolved V in seawater of ~130,000 y with respect to inputs from rivers.
- There they made salt from the seawater and broke a law of British India prohibiting making salt without paying taxes, so this event is referred to as the Salt March.
- Usually, marine light-emission belongs in the blue and green light spectrum, the wavelengths that can transmit through seawater most easily.
- A possible mechanism for the V isotopic offset between seawater and hydrogenous Fe-Mn crusts and nodules is the fractionation during the adsorption of V on the surface of the Fe-Mn oxyhydroxide.
– The amount of oxygen found in seawater depends mostly on the plants growing in it.
– They are filled with seawater during high tides, and exist as separate pools at low tide.
– The abundance of CO2 makes seawater look like a good alternative fuel source.
– Cold seeps change the shape of the ocean floor over time, where reactions between methane and seawater create carbonate rock formations and reefs.
– On the afternoon of July 12, Louisiana Highway 1 south of Golden Meadow—the only thoroughfare leading out of Grand Isle and Port Fourchon—was closed after seawater began to inundate portions of the road.
– The Phoenicians were some of the first to figure out how to do this, by pouring seawater on dry land.