Fifteen-years of continuous application of organic materials improve the soil aggregation, organic carbon status and sustain the productivity of the basmati rice-wheat system

The rice-wheat cropping system covers a considerable area of the Indo-Gangetic Plain zone (IGPZ) due to agro-pedological compatibility. The nutrient requirements of the rice-wheat system in an organic mode are met through locally available organic matter (OM) is a subject of investigation from the v...

Full description

Saved in:
Bibliographic Details
Published inSoil & tillage research Vol. 239; p. 106058
Main Authors Mandi, Sunil, Shivay, Yashbir Singh, Chakraborty, Debashish, Shrivastava, Manoj, Nayak, Somanath, Baral, Kirttiranjan, Reddy, Kadapa Sreenivasa
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2024
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:The rice-wheat cropping system covers a considerable area of the Indo-Gangetic Plain zone (IGPZ) due to agro-pedological compatibility. The nutrient requirements of the rice-wheat system in an organic mode are met through locally available organic matter (OM) is a subject of investigation from the viewpoint of declining the underlying mechanisms. A long-term organic farming experiment was carried out at the research farm of ICAR-Indian Agricultural Research Institute, New Delhi, India. Locally available sources of OM’s such as Sesbania green manuring, Leucaena green leaf manuring, farmyard manure (FYM), blue-green algae, and Azotobacter were evaluated for changes in soil physico-chemical properties and crop yield response after 15 years continuous applied of OM’s. Our results indicate that treatment involving applied Sesbania green manure + farmyard manure + blue-green algae to rice + Leucaena green leaf manuring + farmyard manure + Azotobacter to wheat [SFB(R) + LFA(W)] showed a sharp decline in soil pH by 5.5%, soil electrical conductivity (EC) by 24.0%, and soil bulk density by 14.0% over the control within the 0–15 cm soil depth. While, the treatment SFB(R) + LFA(W) improved the soil large macroaggregate (>2.0 mm) by 85.0% in 0–7.5 cm, and 92.8% in 7.5–15 cm in soil depth. Similarly, the treatment SFB(R) + LFA(W) showed 3.2-, 2.8-fold higher mean weight diameter (MWD) in corresponding soil depths of 0–7.5 cm, 7.5–15 cm compared to the control. Treatment SFB(R) + LFA(W) increased in soil organic carbon (SOC) holding by 5-folds in soil large macroaggregate, 4-folds by soil small macroaggregate (2.0–0.25 mm), 5-folds by micro-aggregate (0.25–0.053 mm), and 9-folds by silt + clay fraction (<0.053 mm) than control in 0–15 cm soil depth. These observations strongly support greater carbon recalcitrance with a higher half-life in soil silt + clay fraction than in other soil fractions. Further, treatment SFB(R) + LFA(W) maintained higher SOC by 79.4% and carbon stock by 76.6% over control in 0–15 cm soil depth. These responses on soil aggregates and SOC changes translated into significant crop responses. The treatment SFB(R) + LFA(W) thus, showed correspondingly higher grain yield (5.41 Mg ha–1 and 4.69 Mg ha–1) of rice and wheat. Our study though showed on par agronomic response between low-quality OM’s and mixed-quality OM’s in 15-years. But considering the loading of SOC in the silt + clay fraction of soil, the study foresees a higher recalcitrant of SOC compared to any other soil fractions. This could well strengthen the process of soil aggregation having cascading response on other soil health-defined parameters a requisite for sustaining the rice-wheat sequence in the IGPZ. •15-year application of organic materials (OM’s) improves soil properties.•Applied mixed-quality OM’s had decreased the soil bulk density, EC, and pH.•Applied mixed-quality OM’s significantly increased the MWD and soil aggregation.•The soil small macroaggregate found a higher organic carbon holding in the plough layer.•The mixed-quality OM’s recorded a 54.78 Mg ha–1 carbon stock in the plough layer.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0167-1987
1879-3444
DOI:10.1016/j.still.2024.106058