2012
DOI: 10.1016/j.fcr.2012.01.013
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Effect of tillage on soil and crop properties of wet-seeded flooded rice

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Cited by 61 publications
(27 citation statements)
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“…Our results suggest that T2 and T5 have a relatively positive effect on soil ρb. In contrast, other studies have reported higher ρb under NT at 0-5 cm depth compared to CT in cropping systems other than RRS [35,38,39]. Soil pH is an important soil quality factor affected by farmers practice and its modifications in the present study ( Figure 1B).…”
Section: Bulk Density and Soil Phcontrasting
confidence: 52%
See 1 more Smart Citation
“…Our results suggest that T2 and T5 have a relatively positive effect on soil ρb. In contrast, other studies have reported higher ρb under NT at 0-5 cm depth compared to CT in cropping systems other than RRS [35,38,39]. Soil pH is an important soil quality factor affected by farmers practice and its modifications in the present study ( Figure 1B).…”
Section: Bulk Density and Soil Phcontrasting
confidence: 52%
“…In a study in Bangladesh, minimum tillage unpuddled transplanting had no negative effect on rice yields across seasons and years, but reduced the time taken for land preparation and crop establishment and decreased the cost of production [9]. The negative effects of RT/NT on crop growth do not necessarily become concerns in wet-seeded flooded rice production systems [39]. The increase in rice yield in the present study may not only be due to tillage, but also due to the combined effect of conservation tillage, residue and nutrient management practices.…”
Section: Economic Productivitymentioning
confidence: 99%
“…Soil aeration is low in continuous rice cropping systems due to water logging. NT can further exacerbate the low soil aeration through increasing soil compaction and decreasing soil porosity (Huang et al, 2012b). As compared with continuous rice cropping systems, rice-upland rotations can lead to an increase in soil porosity within rice-growing season (Huang and Ding, 1995), which may to some extent offset the decreased soil porosity by NT.…”
Section: Resultsmentioning
confidence: 99%
“…The presence of crop residues over the soil surface prevents aggregate breakdown by direct raindrop impact as well as by rapid wetting and drying of soils. There are also reports showing slight or no differences in D b values between CT and ZT in the surface soil layers [58][59][60]. At 11-15-cm and 16-20-cm depths, D b was significantly higher in T1, T2, T3 and T4 than in ZT-DSR (T5 and T6).…”
Section: Soil Physical Parameters Soil Bulk Density (D B )mentioning
confidence: 89%