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Principle and application of AMS .. Reporting 14C activities and concentrations . Thequestion of isotope fractionation .. Thequestion of radioactive decay . Definition of the14C standard activity .

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Oceanography and atmospheric research .. Enhanced 14C radioactivity Origin and characteristics .

Experimental and technical aspects . Mass spectrometric measurement of 3H through 3He .. Natural abundance and isotope fractionation .. Origin and characteristics .. Experimental and technical aspects .. Natural abundance and applications . Origin and characteristics Experimental and technical aspects Significant figures and digits Instrumental uncertainties The Global Cycle of water 1. Introduction Theglobal hydrological cycle together with its driving force, solar radiation, forms thebasic resource for primary biological production.

It provides thewater that is required for theassimilation of carbon and plays an important role in thesupply of nutrients and their transport.

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Moreover, thehydrological cycle is responsible for themoderate and favourable temperature conditions prevailing on Earth through its linkage with theglobal atmospheric cycle. Thehydrosphere is theinterconnection between thebiosphere, theatmosphere and thelithosphere, notably integrating the fluxes of water, energy and geochemical compounds.

All these properties are related to thehigh cohesion and pseudo-crystalline structure of water. This structure is caused by theeccentricity of thepositive hydrogen nuclei with respect 1 to theelectrons and theoxygen nucleus, which gives theH2O molecule an electrical polarity or dipole character.

In this chapter we will discuss thecomposition of thehydrosphere and thebasic concepts of thehydrological cycle and its interaction with atmospheric circulation. Subsequently, we will consider theindividual elements of thehydrological cycle, and their mutual interaction. Finally, attention is paid to theimpact of climatic change and mans interference with thehydrological cycle.

Origin of water on Earth Most probably water has been in our solar system from thebeginning and was formed by thethermonuclear fusion process that produced theelements of theperiodic system and their compounds. Thetotal amount of water contained on Earth is estimated at some 0.

Environmental Isotopes in the Hydrological Cycle Vol 1

Most of this water is chemically and physically bound in rocks and minerals within thecrust and mantle. Theamount of free water, forming thehydrosphere, is estimated at 1. It is generally accepted that most of thewater in thehydrosphere has originated from degassing of theEarths mantle by volcanic eruptions and surfacing lava basalt in thecourse of the5 billion years of theEarths existence. However, it is known that Earth is also exposed to collisions with cosmic material, including ice comets.

An extraterrestrial origin of at least part of theEarths water is therefore likely. Some of theother planets satellites and many comets consist almost completely of ice. Awell-known example is Halleys Comet plus.

On theother hand, asmaller quantity escapes into space and another unknown amount returns to themantle through plate-tectonic processes. This process is driven by thermal convection currents, which move therigid lithosphere as acoherent layer over themore plastic asthenosphere Fig. Magma moves upward into fractures spreading centres in the ocean floor, where it forms new oceanic crust. This causes thelithosphere to move away from thespreading centre.

At theother limb of theconvection cell, thelithosphere sinks downward in asubduction zone. Where old lithosphere disappears in themantle, ocean water is dragged with thecrust to depths of hundreds of kilometres and becomes involved in there-melting of sediments into new magma. Another part of this water is exhaled again by theassociated volcanic and magmatic activity.

This entire process is referred to as thehydrotectonic cycle. This cycle acts on ageologic time scale of millions of years and is quantitatively negligible compared to theamount and distribution of water in thepresent hydrological circulation at theEarths surface and thelower atmosphere.

Thedifference in dynamics of this hydrological cycle and thehydro-tectonic cycle is also reflected in therespective energy fluxes involved.

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Thedriving force behind thehydrological cycle, solar radiation, produces aflux at theEarths surface of 5. Thevolcanic and magmatic exhalations, however, do have aqualitative effect on thehydrosphere by producing chemical compounds and concentrated heat.

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Volcanic dust and gases may influence theEarths heat balance and Fig. Schematic representation of thehydro-tectonic cycle, showing across-section through an ocean-continent boundary.

Theupward moving mantle material forces theoceanic crust to slide under to subduct thecontinental crust. Topography driven flow meteoric water 5. Orbit Downloader is a free social music,video and file downloader. Download is an administrator of downloading. Articles dans la catgorie Tlchargement Browser le navigateur web mobile dpasse les.

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