Knowledge Center Catalog

Local cover image
Local cover image

Short-term (5 years) impact of conservation agriculture on soil physical properties and organic carbon in a rice–wheat rotation in the Indo-Gangetic plains of Bihar

By: Contributor(s): Material type: ArticleArticleLanguage: English Publication details: United Kingdom : Wiley, 2019.ISSN:
  • 1351-0754
Subject(s): In: European Journal of Soil Science In pressSummary: Short-term (5 years) impact of tillage and residue management practices on physical properties and organic carbon (OC) of a silty clay soil was evaluated in a rice?wheat rotation in the Indo-Gangetic Plains of Bihar. The experiment had three conservation agriculture (CA) practices: one full (direct-seeded rice (DSR)?no-tilled wheat (NTW)?no-tilled mung bean (NTMB); fCA) and two partial (puddled transplanted rice (PTR)?NTW?conventionally tilled mung bean (CTMB); pCA1 and unpuddled transplanted rice (UPTPR)?conventionally tilled potato+maize (CTP + M)?NTMB; pCA2), which were evaluated against full conventional practice (puddled transplanted rice (PTR)?conventionally tilled wheat (CTW); TA). Subsurface compaction reduced and soil aggregation improved under both full and partial CA. Macro- and water-stable aggregates increased to a large extent (26 and 11%, respectively) in full CA and to a lesser extent in partial CA, mostly due to increase in coarse macroaggregate (2?8 mm) contents in the 0?10 and 10?20-cm depth soil layers. Steady-state infiltration rate nearly doubled under full CA, with larger pore volume recorded in 10?20 and 20?30-cm depth soil layers. The CA increased OC associated with all size fractions of aggregates in the surface soil layer (0?10 cm), but a higher amount of C was associated with macroaggregates, indicating relative stabilization of OC in the soil under CA. Change in bulk soil OC was larger in the 0?10-cm depth soil layer in favour of CA, which also had an 11% increase in OC stock in the 0?30-cm depth soil layer. Improvement in soil physical condition did not effectively translate into increased rice or wheat yields, but the system productivity increased largely. Highlights: Conservation agriculture (CA) resulted in 11?12% higher macro-aggregation compared to conventional practice (CT). Macro- and total pores reduced in the 0?10 cm depth soil layer but increased in the 10?20 cm depth soil layer under CA. CA resulted in 27?35% higher aggregate-associated OC content and 11% increase in OC stock at 0?30 cm. Full/partial CA improved soil physical condition and the productivity of rice?wheat systems in the Indo-Gangetic Plains.
Tags from this library: No tags from this library for this title. Log in to add tags.
Star ratings
    Average rating: 0.0 (0 votes)
Holdings
Item type Current library Collection Call number Status Date due Barcode Item holds
Article CIMMYT Knowledge Center: John Woolston Library CIMMYT Staff Publications Collection Available
Total holds: 0

Peer review

Short-term (5 years) impact of tillage and residue management practices on physical properties and organic carbon (OC) of a silty clay soil was evaluated in a rice?wheat rotation in the Indo-Gangetic Plains of Bihar. The experiment had three conservation agriculture (CA) practices: one full (direct-seeded rice (DSR)?no-tilled wheat (NTW)?no-tilled mung bean (NTMB); fCA) and two partial (puddled transplanted rice (PTR)?NTW?conventionally tilled mung bean (CTMB); pCA1 and unpuddled transplanted rice (UPTPR)?conventionally tilled potato+maize (CTP + M)?NTMB; pCA2), which were evaluated against full conventional practice (puddled transplanted rice (PTR)?conventionally tilled wheat (CTW); TA). Subsurface compaction reduced and soil aggregation improved under both full and partial CA. Macro- and water-stable aggregates increased to a large extent (26 and 11%, respectively) in full CA and to a lesser extent in partial CA, mostly due to increase in coarse macroaggregate (2?8 mm) contents in the 0?10 and 10?20-cm depth soil layers. Steady-state infiltration rate nearly doubled under full CA, with larger pore volume recorded in 10?20 and 20?30-cm depth soil layers. The CA increased OC associated with all size fractions of aggregates in the surface soil layer (0?10 cm), but a higher amount of C was associated with macroaggregates, indicating relative stabilization of OC in the soil under CA. Change in bulk soil OC was larger in the 0?10-cm depth soil layer in favour of CA, which also had an 11% increase in OC stock in the 0?30-cm depth soil layer. Improvement in soil physical condition did not effectively translate into increased rice or wheat yields, but the system productivity increased largely. Highlights: Conservation agriculture (CA) resulted in 11?12% higher macro-aggregation compared to conventional practice (CT). Macro- and total pores reduced in the 0?10 cm depth soil layer but increased in the 10?20 cm depth soil layer under CA. CA resulted in 27?35% higher aggregate-associated OC content and 11% increase in OC stock at 0?30 cm. Full/partial CA improved soil physical condition and the productivity of rice?wheat systems in the Indo-Gangetic Plains.

Text in English

Click on an image to view it in the image viewer

Local cover image

International Maize and Wheat Improvement Center (CIMMYT) © Copyright 2021.
Carretera México-Veracruz. Km. 45, El Batán, Texcoco, México, C.P. 56237.
If you have any question, please contact us at
CIMMYT-Knowledge-Center@cgiar.org