Soil aggregate-associated carbon and organic carbon pools as affected by conversion of forest lands to agriculture in an acid soil of India

被引:12
|
作者
Das, Sourav [1 ]
Bhattacharyya, Ranjan [1 ,2 ]
Das Saha, Namita [2 ]
Ghosh, Avijit [3 ]
Khan, S. A. [2 ]
Ahmed, N. [1 ]
Dey, Abir [1 ]
Bhatia, A. [2 ]
Pramanik, Pragati [4 ]
Kumar, Soora Naresh [2 ]
Agarwal, B. K. [5 ]
Shahi, D. K. [5 ]
机构
[1] ICAR Indian Agr Res Inst, Div Soil Sci & Agr Chem, New Delhi 110012, India
[2] ICAR Indian Agr Res Inst, Div Environm Sci, New Delhi 110012, India
[3] ICAR Indian Grassland & Fodder Res Inst, Jhansi, Uttar Pradesh, India
[4] ICAR Indian Agr Res Inst, Div Agr Phys, New Delhi 110012, India
[5] Birsa Agr Univ, Div Soil Sci & Agr Chem, Ranchi, Bihar, India
来源
SOIL & TILLAGE RESEARCH | 2022年 / 223卷
关键词
Aggregate stability; Labile and recalcitrant C; Alfisol; C sequestration; Rice-based systems; MICROBIAL BIOMASS; MATTER; TILLAGE; SEQUESTRATION; FRACTIONS; TURNOVER; DYNAMICS; LABILE; STABILIZATION; PARTICULATE;
D O I
10.1016/j.still.2022.105443
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Aggregate-associated soil organic carbon (SOC) controls organic carbon stabilization. The research question of this paper was: what were the effects of conversion of forest land uses to agriculture at Ranchi, India on SOC pools, soil aggregation and aggregate-associated C? The samples were taken from six different land uses viz. native forest (NF), agri-horticulture (AH), native grass land (NG), rice-wheat (RW), rice-vegetable (RV) and maize-wheat (MW) from three soil depths (0-15, 15-30 and 30-45 cm). Soil aggregation, SOC pools and aggregate-associated C were determined. Results revealed that SOC concentration in NF was 36%, 67% and 127% higher than RW, RV and MW land uses, respectively, at 0-15 cm depth. The microbial biomass carbon (MBC) was higher in NF land uses than rice-based systems in the soil surface (0-15 cm) due to less disturbance. In surface soils (0-15 cm depth) under NF, the large macroaggregates had 21% and 40% higher SOC concentration than RW and RV, respectively. Similarly, NF soil had larger small macroaggregate-associated C than RW, RV and MW systems in the 0-15 and 15-30 cm layers. This result supports that tillage and regular crop removal under arable (MW, RW and RV) systems adversely affect loss of SOC contents in the surface layers and C storage inside aggregates, both in the 0-15 and 15-30 cm soil layers at Ranchi, India.
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收藏
页数:7
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