湿垃圾沼渣对城市搬迁地土壤水库特征的影响研究
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上海市绿化和市容管理局项目“湿垃圾处置固态残余物资源化利用途径研究”(编号:G200202) 上海市绿化和市容管理局项目“城市污染土壤生态修复关键技术研发与集成应用”(编号:G190202)


Influence of Food Waste Biogas Residue on the Characteristics of Soil Reservoir in Urban Relocation Sites
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    摘要:

    为了解湿垃圾沼渣对城市搬迁地土壤水库库容特征的影响,选择上海典型搬迁地土壤为研究对象,研究添加不同量沼渣对土壤水库总库容、土壤水分现存量、土壤剩余蓄水空间及土壤滞洪库容的影响,并对土壤水库库容与土壤物理性质进行了相关性分析,结果表明:湿垃圾沼渣对搬迁地土壤水库总库容和水分现存量提升显著,且随着沼渣添加量的增加均有增加趋势,其中以添加80%沼渣的土壤水库总库容最佳,添加60%沼渣的土壤水分现存量最佳。湿垃圾沼渣对搬迁地土壤剩余蓄水空间有所降低,其中以60%沼渣土壤剩余蓄水空间最小。添加不同量沼渣对土壤滞洪库容影响不明显,但以添加40%沼渣滞洪库容最佳。不同土壤物理性质影响着不同土壤水库类型,其中土壤水库总库容主要受总孔隙度、毛管孔隙度、最大持水量、毛管持水量、田间持水量及容重影响,土壤水分现存量主要受含水率、容重、最大持水量、毛孔持水量及田间持水量影响,土壤剩余蓄水空间主要受含水率和入渗率影响,土壤滞洪库容主要受非毛管孔隙度影响。

    Abstract:

    In order to understand the impact of biogas residue from food waste on the storage characteristics of soil reservoirs in urban relocation sites, the soil of a typical relocation site in Shanghai was selected as the research object. The effects of adding different amounts of biogas residues on total storage capacity of soil reservoir, soil water existing volume, soil remaining water storage space, soil detention capacity were studied, and the correlation between soil reservoir capacity and soil physics was analyzed. The results showed that the total storage capacity and moisture quantity of the soil reservoir in the relocation area was improved significantly. With the increase of biogas residue added, the total storage capacity of the soil reservoir with 80% biogas residue was the best, and the soil moisture content of the added 60% biogas residue was the best. On the other hand, biogas residue reduced the soil remaining water storage space of the soil in the relocation area, of which 60% of biogas residue was the smallest. The effect of adding different amounts of biogas residue on soil detention reservoir capacity was not apparent, but it was best to add 40% biogas residue storage capacity. The physical properties of different soils affected different types of soil reservoirs. The soil total reservoir capacity was mainly affected by total porosity, capillary porosity, maximum water holding capacity, capillary water holding capacity, field water holding capacity, and bulk density. The soil water existing volume was mainly affected by water content, bulk density, maximum water holding capacity, capillary water holding capacity, and field water holding capacity. The soil remaining water storage space was mainly affected by the water content and infiltration rate, and the soil detention storage was affected primarily by the non-capillary porosity.

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  • 在线发布日期: 2022-09-20
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