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Saline Soils Can Be Ameliorated by Adding Biochar Generated From Rice-Residue Waste

机译:通过添加水稻残留废物产生的生物炭,可以改善盐渍土

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摘要

Information on the effects of biochar on salinity is inadequate, although increasing data have shown that the addition of biochar can improve soil fertility and crop production. Soil samples varying in electrical conductivity (EC) levels (2 (EC2; non-saline control), 8 (EC8), and 16 (EC16) dSm(-1)) collected from a long-term field experiment on irrigation water induced salinity were incubated for 8 weeks with different rates of rice-residue biochar (B0: unamended, B1: 1%, B2: 2%, B4: 4% w/w). Irrespective of salinity, both EC and pH increased with increasing rate of biochar application. Compared with unamended control soil (EC2), cumulative respiration (CR) and microbial biomass carbon (MBC) in EC8 or EC16 soil was lower by 39-63 and 51-71%, respectively. However, addition of biochar at the rate of 2-4% reduced the decrease in CR and MBC either to 21% or similar to unamended non-saline treatment in EC8 soil, respectively. However, the percentage decrease in CR and MBC was reduced to 47 or 21% in EC16 soil, respectively. Contrarily, biochar addition at the rate of 1% in EC8 or EC16 soil did not show a significant increase in CR and MBC compared with non-saline control. Furthermore, at all salinity levels, NO3--N concentrations increase with increasing incubation time and biochar rates, whereas NH4+-N concentrations were greater on day 14 than day 56 of incubation. It may be concluded that application of higher rates of rice-residue biochar (2-4%) will be more effective in reducing the adverse effects of salinity on soil properties.
机译:有关Biochar对盐度的影响的信息不足,尽管增加数据表明,添加生物炭可以改善土壤肥力和作物生产。从电导率(EC)水平(2(EC2;非盐水管),8(EC8)和16(EC16))中不同的土壤样品从灌溉水诱导盐度的长期场实验中收集用不同的水稻 - 残基生物炭孵育8周(B0:未加工,B1:1%,B2:2%,B4:4%w / w)。无论盐度如何,EC和pH都随着BioChar应用的增加而增加。与未来的对照土壤(EC2)相比,EC8或EC16土壤中的累积呼吸(CR)和微生物生物质碳(MBC)分别较低39-63和51-71%。然而,在2-4%的速率下加入生物炭降低Cr和MBC的降低至21%或类似于EC8土壤中未加工的非盐水处理。然而,CR和MBC的百分比分别降低至EC16土壤中的47或21%。相反,EC8或EC16土壤中的1%率加入的生物炭并未显示出与非盐水控制相比的CR和MBC的显着增加。此外,在所有盐度水平,NO 3 - N浓度随着孵育时间和生物浆率的增加而增加,而NH4 + -N浓度在孵育的第14天的第14天较大。可以得出结论,在降低土壤性质对土壤性质的不利影响方面,可以更有效地施加较高的水稻 - 残留生物炭(2-4%)。

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  • 来源
    《Clean》 |2019年第2期|1700656.1-1700656.9|共9页
  • 作者单位

    Punjab Agr Univ Dept Soil Sci Ludhiana 141004 Punjab India;

    Punjab Agr Univ Dept Soil Sci Ludhiana 141004 Punjab India;

    Punjab Agr Univ Dept Soil Sci Ludhiana 141004 Punjab India;

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