Home > Research > Publications & Outputs > Clay minerals-organic matter interactions in re...

Research

Associated organisational unit

Links

Text available via DOI:

View graph of relations

Clay minerals-organic matter interactions in relation to carbon stabilization in soils

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Chapter

Published

Standard

Clay minerals-organic matter interactions in relation to carbon stabilization in soils. / Sarkar, Binoy; Singh, Mandeep; Mandal, Sanchita et al.
The Future of Soil Carbon: Its Conservation and Formation. ed. / Carlos Garcia; Paolo Nannipieri; Teresa Hernandez. Elsevier Inc., 2018. p. 71-86.

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Chapter

Harvard

Sarkar, B, Singh, M, Mandal, S, Churchman, GJ & Bolan, NS 2018, Clay minerals-organic matter interactions in relation to carbon stabilization in soils. in C Garcia, P Nannipieri & T Hernandez (eds), The Future of Soil Carbon: Its Conservation and Formation. Elsevier Inc., pp. 71-86. https://doi.org/10.1016/B978-0-12-811687-6.00003-1

APA

Sarkar, B., Singh, M., Mandal, S., Churchman, G. J., & Bolan, N. S. (2018). Clay minerals-organic matter interactions in relation to carbon stabilization in soils. In C. Garcia, P. Nannipieri, & T. Hernandez (Eds.), The Future of Soil Carbon: Its Conservation and Formation (pp. 71-86). Elsevier Inc.. https://doi.org/10.1016/B978-0-12-811687-6.00003-1

Vancouver

Sarkar B, Singh M, Mandal S, Churchman GJ, Bolan NS. Clay minerals-organic matter interactions in relation to carbon stabilization in soils. In Garcia C, Nannipieri P, Hernandez T, editors, The Future of Soil Carbon: Its Conservation and Formation. Elsevier Inc. 2018. p. 71-86 doi: 10.1016/B978-0-12-811687-6.00003-1

Author

Sarkar, Binoy ; Singh, Mandeep ; Mandal, Sanchita et al. / Clay minerals-organic matter interactions in relation to carbon stabilization in soils. The Future of Soil Carbon: Its Conservation and Formation. editor / Carlos Garcia ; Paolo Nannipieri ; Teresa Hernandez. Elsevier Inc., 2018. pp. 71-86

Bibtex

@inbook{76e708cfebb942bb83aa1f556bbaa2a8,
title = "Clay minerals-organic matter interactions in relation to carbon stabilization in soils",
abstract = "Stabilization of C in soil is important for minimizing greenhouse gas emission into the atmosphere and for improving the soil fertility. The physical, chemical, and biological properties of soil greatly influence the C protection capacity. Both the physical and chemical properties of soils are directly or indirectly governed by clay minerals, which are the most reactive soil particles. Apart from the amount of clays, clay types are also very important in protecting soil C. Clay minerals provide both permanent and variable surface charges and different specific surface areas that are crucial to determine the C protection capacity of soils. They form organo–mineral complexes, promote aggregate establishment, and protect soil organic matter against microbial decomposition. This chapter aims to provide an overview of the role of various clay minerals in protecting organic C in soils and highlights the mechanisms of C sequestration by clay minerals.",
author = "Binoy Sarkar and Mandeep Singh and Sanchita Mandal and Churchman, {Gordon J.} and Bolan, {Nanthi S.}",
year = "2018",
month = apr,
day = "13",
doi = "10.1016/B978-0-12-811687-6.00003-1",
language = "English",
isbn = "9780128116876",
pages = "71--86",
editor = "Carlos Garcia and Paolo Nannipieri and Teresa Hernandez",
booktitle = "The Future of Soil Carbon",
publisher = "Elsevier Inc.",
address = "United States",

}

RIS

TY - CHAP

T1 - Clay minerals-organic matter interactions in relation to carbon stabilization in soils

AU - Sarkar, Binoy

AU - Singh, Mandeep

AU - Mandal, Sanchita

AU - Churchman, Gordon J.

AU - Bolan, Nanthi S.

PY - 2018/4/13

Y1 - 2018/4/13

N2 - Stabilization of C in soil is important for minimizing greenhouse gas emission into the atmosphere and for improving the soil fertility. The physical, chemical, and biological properties of soil greatly influence the C protection capacity. Both the physical and chemical properties of soils are directly or indirectly governed by clay minerals, which are the most reactive soil particles. Apart from the amount of clays, clay types are also very important in protecting soil C. Clay minerals provide both permanent and variable surface charges and different specific surface areas that are crucial to determine the C protection capacity of soils. They form organo–mineral complexes, promote aggregate establishment, and protect soil organic matter against microbial decomposition. This chapter aims to provide an overview of the role of various clay minerals in protecting organic C in soils and highlights the mechanisms of C sequestration by clay minerals.

AB - Stabilization of C in soil is important for minimizing greenhouse gas emission into the atmosphere and for improving the soil fertility. The physical, chemical, and biological properties of soil greatly influence the C protection capacity. Both the physical and chemical properties of soils are directly or indirectly governed by clay minerals, which are the most reactive soil particles. Apart from the amount of clays, clay types are also very important in protecting soil C. Clay minerals provide both permanent and variable surface charges and different specific surface areas that are crucial to determine the C protection capacity of soils. They form organo–mineral complexes, promote aggregate establishment, and protect soil organic matter against microbial decomposition. This chapter aims to provide an overview of the role of various clay minerals in protecting organic C in soils and highlights the mechanisms of C sequestration by clay minerals.

U2 - 10.1016/B978-0-12-811687-6.00003-1

DO - 10.1016/B978-0-12-811687-6.00003-1

M3 - Chapter

AN - SCOPUS:85058981378

SN - 9780128116876

SP - 71

EP - 86

BT - The Future of Soil Carbon

A2 - Garcia, Carlos

A2 - Nannipieri, Paolo

A2 - Hernandez, Teresa

PB - Elsevier Inc.

ER -