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Titlebook: Biogeochemistry of the Critical Zone; Adam S. Wymore,Wendy H. Yang,Jon Chorover Book 2022 Springer Nature Switzerland AG 2022 Biogeochemis

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期刊全稱Biogeochemistry of the Critical Zone
影響因子2023Adam S. Wymore,Wendy H. Yang,Jon Chorover
視頻videohttp://file.papertrans.cn/188/187053/187053.mp4
發(fā)行地址Combines biogeochemistry with critical zone science.Highlights recent advances in biogeochemistry focusing on CZ sciences.Covers both terrestrial and aquatic systems
學(xué)科分類Advances in Critical Zone Science
圖書封面Titlebook: Biogeochemistry of the Critical Zone;  Adam S. Wymore,Wendy H. Yang,Jon Chorover Book 2022 Springer Nature Switzerland AG 2022 Biogeochemis
影響因子.This book highlights recent advances in the discipline of biogeochemistry that have directly resulted from the development of critical zone (CZ) science. The earth‘s critical zone (CZ) is defined from the weathering front and lowest extent of freely circulating groundwater up through the regolith and to the top of the vegetative canopy. The structure and function of the CZ is shaped through tectonic, lithologic, hydrologic, climatic, and biological processes and is the result of processes occurring at multiple time scales from eons to seconds. The CZ is an open system in which energy and matter are both transported and transformed. Critical zone science provides a novel and unifying framework to consider those coupled interactions that control biogeochemical cycles and fluxes of energy and matter that are critical to sustaining a habitable planet.??.Biogeochemical processes are at the heart of energy and matter fluxes through ecosystems and watersheds. They control thequantity and quality of carbon and nutrients available for living organisms, control the retention and export of nutrients affecting water quality and soil fertility, and influence the ability for ecosystems to seque
Pindex Book 2022
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https://doi.org/10.1007/978-3-322-85782-8is a natural lab with clear orthogonal gradients of rainfall and substrate age, which afford state-factor based analysis of leaching power as a key driver of soil development with feedbacks to the availability of rock-derived nutrients. Chemical properties from soil profiles collected from minimally
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https://doi.org/10.1007/978-3-663-07982-8d lead to a net source of CO. to the atmosphere. However eroded soil OC sequestered in alluvia and reservoirs could create a net sink for atmospheric CO.. The Intensively Managed Landscape—Critical Zone Observatory (IML-CZO) has provided an opportunity to study the fate of the eroded soil OC. A prel
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https://doi.org/10.1007/978-3-662-32849-1is cycled into secondary compounds and translocated down slopes and through the soil profile by erosion and leaching. Over decades, the slow cycling of organic and occluded P fractions can modulate soil P availability—as can human interactions with the critical zone (e.g., through land-use changes).
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