Repeated freeze–thaw cycles increase extractable, but not total, carbon and nitrogen in a Maine coniferous soil
Author:
Funder
UMaine MAFES
University of Maine
Publisher
Elsevier BV
Subject
Soil Science
Reference29 articles.
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3. Increased nitrogen leaching following soil freezing is due to decreased root uptake in a northern hardwood forest;Campbell;Glob. Chang. Biol.,2014
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1. Soil Open Pore Structure Regulates Soil Organic Carbon Fractions of soil Aggregates under Simulated Freeze‑Thaw Cycles as Determined by X‑ray Computed Tomography;Journal of Soil Science and Plant Nutrition;2024-06-24
2. Divergent controlling factors of freeze–thaw-induced changes in dissolved organic carbon and microbial biomass carbon between topsoil and subsoil of cold alpine grasslands;CATENA;2024-06
3. Effects of reduced snowpack due to climate warming on abiotic and biotic soil properties in alpine and boreal forest systems;PLOS Climate;2024-05-07
4. Effects of snow removal on seasonal dynamics of soil bacterial community and enzyme activity;European Journal of Soil Biology;2023-11
5. Linking soil microbial community to the chemical composition of dissolved organic matter in a boreal forest during freeze–thaw cycles;Geoderma;2023-03
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