meteoric water वाक्य
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- Hutt Lagoon, north of the river mouth, is a marginal marine Carnarvon, Hutt Lagoon is fed by marine waters through a barrier ridge and by meteoric waters through springs.
- The composition of the water in various springs around Taftan varies in terms of elemental composition, probably reflecting the mixing between volcanic and meteoric waters and interaction with host rocks and brines.
- This process of biodegradation occurs close to the earth's surface, where temperatures are low enough for the bacteria to thrive, and where the oil is surrounded by fresh meteoric water.
- It should also be pointed out that a local meteoric water line can have a different slope and intercept from the GMWL, due to differences in humidity and evaporation intensity at different places.
- Sources of hydrothermal solutions include seawater and meteoric water circulating through fractured rock, formational brines ( water trapped within sediments at deposition ) and metamorphic fluids created by dehydration of hydrous minerals during metamorphism.
- The relative enrichment of the heavy isotopes in rainwater ( as referenced to mean ocean water ), when plotted against temperature falls predictably along a line called the global meteoric water line ( GMWL ).
- The value of this " deuterium excess ", as it is called, is about + 10 per mil ( 1 % ) in most meteoric waters and its non-zero value is a direct manifestation of kinetic isotope fractionation.
- The heavy isotopes of hydrogen and oxygen in rainwater ( so-called meteoric water ) are enriched as a function of the environmental temperature of the region in which the precipitation falls ( and thus enrichment is related to mean latitude ).
- Discontinuous sand bodies at the base of the McMurray Formation in the Athabasca Oil Sands region of northeastern Alberta, Canada, are commonly referred to as the formations they are saline, and where they are shallow and recharged by meteoric water they are non-saline.
- Fresh-water aquifers, especially those with limited recharge by snow or rain, also known as meteoric water, can be over-exploited and depending on the local hydrogeology, may draw in non-potable water or saltwater intrusion from hydraulically connected aquifers or surface water bodies.
- More generally, therefore, re-profiling systems are associated with and integrated by surficial protection of the slope against erosion and by regulation of meteoric waters through drainage systems made up of ditches and small channels ( clad or unclad and prefabricated ) to run off the water collected.
- Precipitation of tufa in the Portneuf drainage is produced through the combination of four complex mechanisms : dissolution of limestones by meteoric waters containing carbonic acids, degassing of CO 2 at turbulent sites, the removal of CO 2 by photosynthetic plants, and the trapping of particles of CaCO 3 by the biota.
- The depth of the halocline is a function of several factors : climate and specifically how much meteoric water recharges the aquifer, hydraulic conductivity of the host rock, distribution and connectivity of existing cave systems and how effective these are at draining water to the coast, and the distance from the coast.
- In terrestrial hydrothermal systems, the majority of water circulated within the fumarole and geyser systems is meteoric water plus ground water that has percolated down into the thermal system from the surface, but it also commonly contains some portion of metamorphic water, magmatic water, and sedimentary formational brine that is released by the magma.
- The Rayleigh distillation model can also be used to explain the strong correlation between ?D and ? 18 O observed in global precipitation, expressed as the global meteoric water line ( GMWL ) : ?D = 8? 18 O + 10 ( later updated to ?D = 8.17?.07 ? 18 O + 11.27?.65 ) The slope of the GMWL reflects the relative magnitude of hydrogen and oxygen isotope fractionation during condensation.
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