Sentence examples for mineralization and sequestration from inspiring English sources

In this review, we provide a comprehensive cross-disciplinary review on SOC mineralization and sequestration at sites of erosion, along the transport pathway and at depositional sites.

In this experimental context, resilience of microbial catabolic functions was not observed and in consequence ecosystem processes such as carbon mineralization and sequestration in soil may be affected.

Numerous questions remain to be addressed before determining the C sink/source effect of soil erosion, especially for the mineralization and sequestration of eroded SOC upon erosion, transport and deposition.

The comprehensive understanding of physical, chemical and biological mechanisms affecting the mineralization and sequestration of eroded SOC provides important insights to balance the global carbon budget and finally holds the answer on the carbon sink/source controversy.

The current state of knowledge on the impacts of erosion-induced soil aggregate breakdown and formation, removal of SOC from eroding sites and deep burial of SOC at depositional sites on the mineralization and sequestration of SOC are presented.

The redistribution of soil and associated organic matter across landscape represents a major perturbation to the carbon cycle because the established colluvial soils change the levels of C mineralization and sequestration.

These fractions show an adjusted carbon balance although mineralization and carbon sequestration occurred, confirming other studies [24 26] which state, that the light fraction is not an universal indicator in relation to land use change.

These fractions show an adjusted carbon balance although mineralization and carbon sequestration occurred, confirming other studies [ 24- 26] which state, that the light fraction is not an universal indicator in relation to land use change.

The fraction of plant biomass returned to soil is transformed into more stable humic substances and contributed to the formation of different organo-mineral complexes and microaggregates which protect soil carbon for further mineralization and increase C sequestration (Lal 2016).

Halophilic bacteria or microorganisms that have adapted to high-range salinity-changing environments can be used for the determination of the effect of the ionic characterization of the medium over the bacterial carbonate mineralization and therefore over CO2 sequestration [ 10].

Bacterial components (e.g., cell walls) facilitate mineralization by sequestration of metallic ions from solution and provide local sites for nucleation and growth (Beveridge and Fyfe, 1985).