Fe (hydr) oxides and organic matter (OM) are two of the main active substances ubiquitously
occurring in natural environments. Fe (hydr) oxides rarely exist as a discrete component in …

Iron (Fe) minerals play an important role in stabilizing soil organic carbon (SOC). Fe-
mediated SOC protection is mainly achieved through adsorption, co-precipitation, or …

Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss,
potentially triggering a positive C-climate feedback. However, earlier observations have …

摘要青藏高原是全球中纬度面积最大的多年冻土分布区, 青藏高原多年冻土对东亚季风乃至全球
气候系统都有重要影响. 本文在前人研究成果的基础上, 系统地梳理了青藏高原多年冻土基本 …

Iron (Fe) oxides are widely recognized to prevent the degradation of organic matter (OM) in
environments, thereby promoting the persistence of organic carbon (OC) in soils. Thus …

It has been shown that reactive soil minerals, specifically iron (III)(oxyhydr) oxides, can trap
organic carbon in soils overlying intact permafrost, and may limit carbon mobilization and …

Purpose Soil organic matter is an important part of the earth's carbon cycle, of which stability
is related to its own obstinacy, and environmental disturbance also plays an important role …

Metal‐bound organic carbon (OC) is vital for the persistence of soil organic carbon (SOC).
However, its relative importance in different land types (eg, upland vs. wetland) remains …

Abstract Wetlands in the Yarlung Tsangpo River Basin (YTR) on the Qinghai-Tibet Plateau
provide immense soil organic carbon (SOC) storage, which is highly susceptible to climate …

Reductive dissolution during permafrost thaw releases iron-bound organic carbon to
porewaters, rendering previously stable carbon vulnerable to microbial decomposition and …