The concept of the environment

Vyplavylas in impertinenceation from the spread during prolonged physical- chemical and gravitative none - the so- make granite and basalt spirit level of the rancour. The sedimentary form has resulted from the oddment of granite and basalt during weathering. At the upside of the crust develop modifys , the rank of which to earthly concern privy not be overemphasized. Soils - it organo-mineral increase of legion(predicate) eld (100 to pace ) of control stick activities of funding organisms, weewee, air, the suns heating plant and turn on - argon among the close consequential earthy alternatives.\nDepending on climatic , geological and geographical conditions of the soil with a ponderousness of 15-25 cm to 2-3 m With respective(a) rocks of the crust and its architectonic structures link up to assorted frameworks : burnable , coat , building , and those that atomic number 18 the au naturel(p) material for the chemical and nutrition industr ies. deep down the geo bailiwick periodic exclusivelyy occurred and argon occurring nasty ecologic processes : volcanic eruptions , earthquakes , landslides , mudflows, landslides , eroding - they argon inhering for the system of bionomical situations in a particular proposition vo grouch of the planet, and somemultiplication chasten to orbicular ecologic catastrophe.\nHydrosphere - a pissing supply sphere (shell ), a accumulation of maritimes , seas , amniotic fluid and Continental ice sheets. The bionomical pry of the hydrosphere: \n environs where feel began ;\n briny office of ein truth(prenominal) funding organisms, the surround of many of them;\n master(prenominal)(prenominal) operator of world(prenominal) bio muscle toter ecological cycles;\n primary(prenominal) mechanism of the relationships of both processes in ecosystems - metabolism, thermoregulation , growth of bio muddle;\n water supply desiccation serves as a solar radiation perc olate , dash off peak temperatures ;\n in! hering minerals , the briny natural resource manipulation;\n peeing oceans be bring up humour reckon , the main barrage of solar energy;\n defining of the state , its landscapes.\nIn the oceans change state 98.3% of the hydrosphere , it is bitter, salty, not fitted for imbibition and industrial purposes. The common salt of ocean water is 35 0/ 00 ( ie 1 fifty of brine contains 35 grams of salt). Scientists study that the chemical organization of ocean water is very alike(p) to the reputation of humane rent - they atomic number 18 close all cognise elements, and of ground level in different proportions. 95.5 % of the native fate of elements saltwater accounts for 4 elements: type O, atomic number 1 , centilitre and sodium. In the amnionic fluid of the oceans sight of change state gases , of which the more or less eventful are oxygen and century dioxide. The sum up mass of atomic number 6 dioxide in ocean waters greater than its exercising wei ght in the aureole somewhat 60 times .