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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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樓主: Stenosis
21#
發(fā)表于 2025-3-25 03:31:46 | 只看該作者
Eroded Critical Zone Carbon and Where to Find It: Examples from the IML-CZO,ediments indicate that row crop soils with corn (C4 plant) isotopic signatures contribute to the sequestered C pools but are not the sole sources of OC. C-isotope and biomarker measurements of Lake Decatur sediments reveal the episodic nature of row crop soil OC transport, which appears to be facili
22#
發(fā)表于 2025-3-25 08:03:26 | 只看該作者
23#
發(fā)表于 2025-3-25 15:14:07 | 只看該作者
Hillslope Position and Land-Use History Influence P Distribution in the Critical Zone,r total, bioavailable, and soil solution P concentrations in the historically farmed hillslopes and that P in the subsoil (>1 m) would be elevated in these hillslopes due to P leaching vertically through the soil profile over time. Finally, we expected to find more organic P (P.) in never cultivated
24#
發(fā)表于 2025-3-25 17:16:26 | 只看該作者
2731-5851 nts available for living organisms, control the retention and export of nutrients affecting water quality and soil fertility, and influence the ability for ecosystems to seque978-3-030-95923-4978-3-030-95921-0Series ISSN 2731-5851 Series E-ISSN 2731-586X
25#
發(fā)表于 2025-3-25 21:13:37 | 只看該作者
Book 2022eart 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
26#
發(fā)表于 2025-3-26 01:10:34 | 只看該作者
27#
發(fā)表于 2025-3-26 08:01:30 | 只看該作者
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發(fā)表于 2025-3-26 10:58:54 | 只看該作者
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發(fā)表于 2025-3-26 15:58:59 | 只看該作者
30#
發(fā)表于 2025-3-26 20:38:23 | 只看該作者
Advances in Biogeochemical Modeling for Intensively Managed Landscapes,orm of agricultural practices have induced significant shifts in the transport and transformation of water, carbon, and nutrients across the landscape. Disentangling the present-day complexity of physical, biological, and hydrologic CZ processes in intensively managed landscapes requires us to first
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