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Phosphorus cycle - Wikipedia
The global phosphorus cycle includes four major processes: (i) tectonic uplift and exposure of phosphorus-bearing rocks such as apatite to surface weathering; [ 19 ] (ii) physical erosion, and chemical and biological weathering of phosphorus-bearing rocks to provide dissolved and particulate phosphorus to soils, [ 20 ] lakes and rivers;
The Global Phosphorus Cycle: Past, Present, and Future
The modern terrestrial phosphorus cycle is dominated by agriculture and human activity. The natural riverine load of phosphorus has doubled due to increased use of fertilizers, deforestation and soil loss, and sewage sources.
12.5: The global phosphorus cycle - Geosciences LibreTexts
The Phosphorus Cycle. Phosphorus is an essential nutrient for living processes; it is a major component of nucleic acid s, both DNA and RNA; of phospholipids, the major component of cell membranes; and, as calcium phosphate, makes up the supportive components of our bones.
Phosphorus Cycle – Definition, Steps, Importance, With Diagram
2020年3月3日 · How is the phosphorus cycle different from the other biogeochemical cycles? The global phosphorus cycle differs from other nutrient cycles in that it is a slow process and does not include any gaseous phase – a unique feature of this cycle.
Phosphorus - Understanding Global Change
What is the phosphorus cycle? Phosphorus cycles through both the abiotic and biotic parts of the Earth system, especially in the biosphere, hydrosphere, and geosphere. Phosphorus is found in the Earth’s crust, primarily in sedimentary rocks that contain phosphate (PO 4 3-) minerals.
global phosphorus cycle remain poorly under-stood. Following the overview, various aspects of the global phosphorus cycle will be examined in more depth, including a discussion of the most pressing research questions currently being posed, and research efforts presently underway to address these questions. 8.13.2 THE GLOBAL PHOSPHORUS CYCLE ...
Soluble Reactive Phosphorus (SRP) is measured in filtered seawater as the fraction of phosphate that can be measured directly by the colorimetric phosphomolybdate method. This fraction is believed to consist mainly of inorganic phosphate, but may also encompass some acid-labile organic compounds.
In this article the global biogeochemical cycling of phosphorus is treated from a quantitative angle. Not only the various transfers but also the various inventories of phosphorus have been calcu lated from literature values. The atmospheric part of the phosphorus cycle is largely unknown.
In this paper, I explore the sources, interactions, and even- tual fate of P on Earth from the system perspective. I also outline efforts to understand variations in P cycling, with a look both...
Here we present a compilation of phosphorus abundances in marine sedimentary rocks spanning the past 3.5 billion years. We find evidence for relatively low authigenic phosphorus burial in...