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– In the northeast Pacific Ocean from 0-500m, Nickel concentrations range from 5.54 nmol\/kg of seawater<\/strong><\/strong> to 6.63 nmol\/kg of seawater<\/strong><\/strong>, as there is a region of productivity there.\n<\/p>\n <\/p>\n – This prevents the water in the brine pool from mixing with the ‘normal’ seawater<\/strong> above.\n<\/p>\n <\/p>\n – Chlorine is reacted with seawater<\/strong> to change the iodide to iodine.\n<\/p>\n <\/p>\n – Primary producing prokaryotic communities of brine, interface and seawater<\/strong> above the halocline of deep anoxic lake L’Atalante, Eastern Mediterranean Sea.\n<\/p>\n <\/p>\n – Salt that is gained through evaportation of seawater<\/strong> needs to be cleaned; this is done by dissloving it in brine and then forcing it to crystallize.\n<\/p>\n <\/p>\n – Temporal variations of V in seawater<\/strong> 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.\n<\/p>\n <\/p>\n – This halocline between the seawater<\/strong> 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.\n<\/p>\n – There they made salt from the seawater<\/strong> and broke a law of British India prohibiting making salt without paying taxes, so this event is referred to as the Salt March.\n<\/p>\n <\/p>\n – Usually, marine light-emission belongs in the blue and green light spectrum, the wavelengths that can transmit through seawater<\/strong> most easily.\n<\/p>\n <\/p>\n – A possible mechanism for the V isotopic offset between seawater<\/strong> and hydrogenous Fe-Mn crusts and nodules is the fractionation during the adsorption of V on the surface of the Fe-Mn oxyhydroxide.\n<\/p>\n <\/p>\n – These are the presence of seawater<\/strong> and the presence of enough light for photosynthesis.\n<\/p>\n <\/p>\n – Vanadium is an element that is widely distributed in Earth’s crust as well as in seawater<\/strong> and groundwater reservoirs.\n<\/p>\n <\/p>\n – The fad for bathing in seawater<\/strong> as a cure for illnesses was encouraged.Seldon, Anthony 2002.\n<\/p>\n <\/p>\n – Changes in local redox conditions impart a significant isotopic fractionation from seawater<\/strong> as recorded in the local sedimentary V isotopic signature.\n<\/p>\n <\/p>\n – 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<\/strong> of ~130,000 y with respect to inputs from rivers.\n<\/p>\n <\/p>\n![\"seawater](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/seawater-in-sentences.jpg\" "\\"seawater")
Example sentences of “seawater”:<\/h2>\n
- There they made salt from the seawater<\/strong> and broke a law of British India prohibiting making salt without paying taxes, so this event is referred to as the Salt March.\r\n
- Usually, marine light-emission belongs in the blue and green light spectrum, the wavelengths that can transmit through seawater<\/strong> most easily.\r\n
- A possible mechanism for the V isotopic offset between seawater<\/strong> and hydrogenous Fe-Mn crusts and nodules is the fractionation during the adsorption of V on the surface of the Fe-Mn oxyhydroxide.\r\n
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