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Titlebook: Biological Weathering and the Environment of the Earth; Tasuku Akagi Book 2024 The Editor(s) (if applicable) and The Author(s), under excl

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41#
發(fā)表于 2025-3-28 18:32:58 | 只看該作者
How to Store (or Release) Carbon in (or from) Deep Oceane and absorb CO.. The mechanisms by which oceanic water absorbs CO. are understood through a simple idea: to absorb CO., excess OH. ions produced by weathering are necessary. Additionally, upwelling zones are identified as CO.-releasing zones, where calcification reactions contribute to the CO. rele
42#
發(fā)表于 2025-3-28 22:02:01 | 只看該作者
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發(fā)表于 2025-3-28 23:34:50 | 只看該作者
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發(fā)表于 2025-3-29 03:47:06 | 只看該作者
Book 2024g as a reaction catalyzed by both plants and plankton, occurring not only on land but also ubiquitously in the earth’s environment, including the ocean’s interior. This new and novel perspective has significant implications for various scientific fields, including biology, marine chemistry, environm
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發(fā)表于 2025-3-29 09:46:42 | 只看該作者
2191-0707 ubiquitously in the earth’s environment, including the ocean’s interior. This new and novel perspective has significant implications for various scientific fields, including biology, marine chemistry, environm978-981-97-4428-2978-981-97-4426-8Series ISSN 2191-0707 Series E-ISSN 2191-0715
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發(fā)表于 2025-3-29 15:00:14 | 只看該作者
Biological Weathering and the Environment of the Earth
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發(fā)表于 2025-3-29 18:55:01 | 只看該作者
Book 2024tant processes on Earth because it influences the circulation of elements, including carbon. Weathering has almost always been considered an abiotic process. The book describes the author’s experiments, proving that plant involvement in weathering is a strategy for plants to ingest nutrients from ro
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發(fā)表于 2025-3-29 19:58:08 | 只看該作者
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發(fā)表于 2025-3-30 00:40:12 | 只看該作者
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發(fā)表于 2025-3-30 07:40:31 | 只看該作者
https://doi.org/10.1007/BFb0066739natural consequence of one cycle. Here, we demonstrate that the conventional ice-based model and the carbon-based model can be seamlessly integrated, enhancing our understanding of the features of glacial–interglacial cycles.
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