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General

Portuguese Majesty

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However, the doubt was exactly in the definition of this river, for Brazil, is it always what it drains the West of the handle of Orange. For France, after some hesitations, it was being the call in accordance with fit OAK, 1998, p.197, the D. Joo V, to conclude with Luis XIV (King of France), the Treated one to Utrecht of 1713 (11 of April), being represented Portugal, for conde of Tarouca and D. Luis of the Wedge. Here, translation software expresses very clear opinions on the subject. Thanks to the good crafts of the Queen Ana of England, the Portuguese representatives had gotten some advantages, as the recognition of the two edges of Amazon Portugal (article X); the French resignation to lands of the Amap (article VIII); the interdiction of catequese for French missionaries (article XIII); the prohibition of the Portuguese commerce in Caiena (article XI). still according to Thin Carlos of Oak, was> in order to prevent all the discord occasion, that could have enters the vassals of the Crown of the France and of the Crown of Portugal, Its Cristianssima Majesty will give up forever, as presently it gives up for this treating for the more authentic terms strongest and. continuing, says Rio Branco in its translation of this related article and with all the clauses that if they thus require, as if they were declared here, in its name, as of its descendants, successors and heirs, of all and any right and pretension who can or will be able to have on the property of lands called the situated Handle North and between the River of Amazon and of Vicente Pinzn’ ‘ some of said lands, so that they are possessed daqui ahead for Its Portuguese Majesty, its descendants, successors and heirs, with all the rights of sovereignty, absolute power and entire domain, as part of its States. The river Oiapoque is born in the Mountain range of Tumucumaque and if dirige on-line little sinuosa for the Northwest until its mouth in the Ocean, under the parallel 4 13' 16 ' ' of Norte&#039 Latitude; '. .

General

The Condensation

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The condensation nuclei are formed by some leave hygroscopic that they are originated from the water of the sea, beyond some gases as hygroscopic oxides of sulphur and match that are produced by intermediary of the industrial production or the combustion of gases in centers highly urbanizados. It fits to stand out, that nor all the originated oxides of the industrial process and nor so little the common toxic dust in great centers with high intensity of vehicles go to generate condensation nuclei. The formation of hygroscopically active nuclei of condensation occurs when, according to Tubelis (1980, p.167) ‘ ‘ the relative humidity of air reaches one definitive value, that in some cases can be so low how much 70%’ ‘. Soon, (Ibid, p.168) ‘ ‘ when become assets, the nuclei start to adsorver vapor molecules d? water, increasing of size and reducing the visibility, giving origin to a mist mida’ ‘. The existence of hygroscopic particles in suspension in the atmosphere are an essential condition for the cloud formation, that beyond this element needs great amount of vapor d directly? water in suspension in the atmosphere, that later will go to cool itself from the moment that suffers adiabtica expansion. These, therefore, are the necessary elements for the formation of a cloud, that can have origin through the thermal convection for adiabtica expansion, or for intermediary of the rise of the relief, as well as, of the shock between front of air mass de with distinct thermal characteristics and humidity. The rocking of solar radiation of the Land is related the factors that influence directly in the interaction of the solar ray with the terrestrial surface, such factors is the surface distribution eliminates and continental as well as the aspects of the same ones, the period of the day, the period of the year, the latitude, at last, in the terrestrial surface meets distributed zones of thermal behavior with distinct, resultant characteristics however of positive rockings of energy as in the tropical zones, or of negative rockings of radiation as in the polar zones.