The rate at which soil organic matter, SOM, is decomposed is temperature dependent and a source of greenhouse gases to the atmosphere (Brinkman and Sombroek, …
WhatsApp: +86 18221755073We found that the higher level of Q10 was in deeper soil, reflecting the distinct SOC formation mechanisms at different depths. Mineral-bound organic compounds derived from plant …
WhatsApp: +86 18221755073While soil organic carbon (C) decomposition is generally thought to increase with temperature 1, 2, recent studies have postulated that this may be a temporary effect, …
WhatsApp: +86 18221755073The objectives of this study are to explore the effect of different forms of straw from the same source on the temperature sensitivity of soil organic carbon (SOC) mineralization in …
WhatsApp: +86 18221755073We conclude that important advances in understanding the temper-ature response of the processes that control substrate availability, depolymerization, microbial efficiency, and …
WhatsApp: +86 18221755073We show that the lower the rate of respiration at a reference temperature of 20 °C—and thus the more biogeochemically recalcitrant the organic matter—the greater the …
WhatsApp: +86 18221755073Temperature sensitivity (Q10) of soil organic matter (SOM) decomposition is a crucial parameter for predicting the fate of soil carbon (C) under global warming.
WhatsApp: +86 18221755073While soil organic carbon (C) decomposition is generally thought to increase with temperature 1, 2, recent studies have postulated that this may be a temporary effect, potentially mitigating...
WhatsApp: +86 18221755073Temperature sensitivity (Q10) of soil organic matter (SOM) decomposition is a crucial parameter for predicting the fate of soil carbon (C) under global warming.
WhatsApp: +86 18221755073Understanding the temperature sensitivity (Q 10) of soil organic matter (SOM) decomposition is crucial to predict CO 2 emissions and carbon (C) stocks under global warming.
WhatsApp: +86 18221755073Understanding the temperature sensitivity (Q 10) of soil organic matter (SOM) decomposition is crucial to predict CO 2 emissions and carbon (C) stocks under global warming.
WhatsApp: +86 18221755073Here, we focused on three main grassland types (alpine meadow, steppe, and desert) and conducted a soil incubation experiment at five different temperatures (5, 10, 15, 20, and 25°C) …
WhatsApp: +86 18221755073Global temperature rise and increasing drought severity are now indisputable realities, making soil organic carbon cycling under climate warming a critical research priority. …
WhatsApp: +86 18221755073Global temperature rise and increasing drought severity are now indisputable realities, making soil organic carbon cycling under climate warming a critical research priority. …
WhatsApp: +86 18221755073Copyright © 2024.FIXIN All rights reserved.sitemap