Organic matter decomposition is a biochemical process with consequences affecting climate
change and ecosystem productivity. Once decomposition begins, C is lost as CO 2 or …

Soils comprise the largest terrestrial carbon (C) pool, containing both organic and inorganic
C. Soil inorganic carbon (SIC) was frequently disregarded because (1) it is partly heritage …

Изложена эко-био-физико-химическая концепция происхождения, образования,
состава, свойств и функций почвенного органического вещества и его стабильной …

Understanding the alterations in soil microbial communities in response to climate warming
and their controls over soil carbon (C) processes is crucial for projecting permafrost C …

Soil contains approximately 2344Gt (1 gigaton= 1 billion tonnes) of organic carbon globally
and is the largest terrestrial pool of organic carbon. Small changes in the soil organic carbon …

Globally, substantial quantities of organic amendments (OAs) such as plant residues (3.8×
10 9 Mg/yr), biosolids (10× 10 7 Mg/yr), and animal manures (7× 10 9 Mg/yr) are produced …

This review evaluates the importance of root exudates in determining rhizosphere bacterial
community structure. We present evidence that indicates that:(1) the direct influence of root …

The loss of organic and inorganic carbon from roots into soil underpins nearly all the major
changes that occur in the rhizosphere. In this review we explore the mechanistic basis of …

Living roots and their rhizodeposits affect microbial activity and soil carbon (C) and nitrogen
(N) mineralization. This so-called rhizosphere priming effect (RPE) has been increasingly …

Plant functional traits control a variety of terrestrial ecosystem processes, including soil
carbon storage which is a key component of the global carbon cycle. Plant traits regulate net …