Titlebook: Weathering and the Riverine Denudation of Continents; Pedro José Depetris,Andrea Inés Pasquini,Karina Le Book 2014 The Author(s) 2014 Diss

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Introduction, landscape. Clearly, the wearing away of the Earth’s surface cannot occur unless a series of synergistic processes, collectively known as “weathering,” are initiated. This term, in use for a long time, promotes the idea that climate (weather) always plays a major role in rock breakdown; since this i

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The Commencement of Continental Denudation: Mechanical Weathering,quent commencement of continental denudation. The action of temperature, humidity, and pressure interact to breakdown minerals and rocks, thus increasing the specific surface and facilitating the action (subsequent or concurrent) of biological and chemical agents. In order to understand the processe

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The Commencement of Continental Denudation: Mechanical Weathering,quent commencement of continental denudation. The action of temperature, humidity, and pressure interact to breakdown minerals and rocks, thus increasing the specific surface and facilitating the action (subsequent or concurrent) of biological and chemical agents. In order to understand the processe

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The Biological Path to Rock Breakdown,gy, it is now possible to attain a more accurate view on the role of biology in the breakdown of minerals and rocks in the Earth’s material cycle. Roots, lichens, mosses, algae, and bacteria are significant agents in mineral and rock breakdown, even exerting in some cases a comminuting action that p

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The Biological Path to Rock Breakdown,gy, it is now possible to attain a more accurate view on the role of biology in the breakdown of minerals and rocks in the Earth’s material cycle. Roots, lichens, mosses, algae, and bacteria are significant agents in mineral and rock breakdown, even exerting in some cases a comminuting action that p

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,Chemical Weathering Processes on the Earth’s Surface,tremely different from those prevailing during their formation, with higher temperature, pressure, and often exposed to chemically aggressive fluids. The processes involved in chemical weathering, such as dissolution, hydrolysis, etc., are at the core of the adjustment mechanism, transforming solid,

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,Chemical Weathering Processes on the Earth’s Surface,tremely different from those prevailing during their formation, with higher temperature, pressure, and often exposed to chemically aggressive fluids. The processes involved in chemical weathering, such as dissolution, hydrolysis, etc., are at the core of the adjustment mechanism, transforming solid,

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