HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Murage, E. W. Articles by Beyaert, R. P. Search for Related Content PubMed Articles by Murage, E. W. Articles by Beyaert, R. P. Agricola Articles by Murage, E. W. Articles by Beyaert, R. P. Related Collections Soil Organic Matter Carbon Sequestration Tillage

SOIL & WATER MANAGEMENT & CONSERVATION

Dynamics and Turnover of Soil Organic Matter as Affected by Tillage

^a Dep. of Land Resource Science, Univ. of Guelph N1G 2W1, Guelph, ON, N1G 2W1, Canada
^b Agriculture and Agri-Food Canada, N5V 4T3, 1391 Sandford St., London, ON, N5V 4T3, Canada

^* Corresponding author (eodoi{at}charter.net).

Greater knowledge of the dynamics of organic matter in different locations in the soil matrix can provide valuable information for implementing tillage practices that may favor C sequestration and improve soil quality. The objective of this study was to investigate the effect of tillage practices on the dynamics and turnover of organic matter located outside (free light fraction [FLF]) and inside (occluded light fraction [OLF]) aggregates, and in intimate association with soil minerals (heavy fraction [HF]). Composite soil samples from 11-yr-old corn (Zea mays L.) plots under no-till (NT) and conventional tillage (CT) practices, and from >60-yr-old tobacco (Nicotiana tabacum L.)–rye (Secale cereale L.) plots under CT were fractionated into these fractions, and changes in the amounts of total soil organic C (SOC), corn-derived (C₄) C, and native (C₃) C and the turnover of native C as a consequence of tillage were estimated. Adoption of NT increased (P < 0.05) standing SOC and C₄–C stocks in whole soil and all its density fractions in the 0- to 5-cm depth, but it did not alter these in the plow layer (0–20-cm soil depth), indicating that NT primarily redistributed C within the profile without necessarily increasing SOC storage. Relative to CT, NT slowed the turnover of native C by 1.5 times and marginally (P = 0.1) increased the sequestration of C₄–C by 23% in the plow layer in OLF only; however, C₃– and C₄–C of OLF accounted for only small (6–10%) proportions of the soil's C₃– and C₄–C. Therefore, NT did not result in increased SOC sequestration in the plow layer.

Abbreviations: CT, conventional tillage • C₃–C, native C • C₄–C, corn-derived C • FLF, free light fraction • HF, heavy fraction • LF, light fraction • NT, no-till • OLF, occluded light fraction • SOC, soil organic carbon • SOM, soil organic matter