凍融對污染土壤中重金屬穩(wěn)定化性能影響研究
本文選題:凍融循環(huán) 切入點(diǎn):重金屬 出處:《遼寧工程技術(shù)大學(xué)》2015年碩士論文 論文類型:學(xué)位論文
【摘要】:為了分析凍融前后對污染土壤中的重金屬穩(wěn)定化后性能的影響,選取赤泥和硫化鈉作為添加劑對土壤中的Pb、Zn和Cd進(jìn)行穩(wěn)定化處理。通過模擬凍融過程,分析凍融循環(huán)后重金屬的浸出毒性、生物可給性、土壤pH和土壤結(jié)構(gòu)的變化,通過力學(xué)滲透實(shí)驗(yàn)考查穩(wěn)定化土壤,經(jīng)過凍融處理前后的變化趨勢,借助X射線衍射與掃描電鏡來探討凍融循環(huán)對穩(wěn)定化處理土壤中重金屬長期穩(wěn)定性能的影響。結(jié)果表明:穩(wěn)定化處理的土壤中Pb、Zn和Cd的浸出毒性分別比原始污染土降低了98.5%、99.8%和99.7%。養(yǎng)護(hù)30d后,Zn和Cd的生物可給性由28.8%和49.5%降到11.5%和21.8%,Pb的生物可給性由52.9%升到57.9%。預(yù)測Pb、Zn和Cd在土壤中的釋放特征,探討了經(jīng)過60次凍融循環(huán)后3種土壤重金屬穩(wěn)定性的變化,其中Cd、Pb和Zn的浸出毒性與穩(wěn)定化后樣品相比增加了4.27、2.47和89.7mg/L,生物可給性比未凍融樣品略有增高。隨著養(yǎng)護(hù)時(shí)間與凍融時(shí)間的增長,土壤pH值呈現(xiàn)升高趨勢。不同階段土壤掃描電鏡圖片可以清晰的觀察到不斷的凍融循環(huán)迫使土壤空隙變大,結(jié)構(gòu)松散。定性和定量分析結(jié)果表明凍融過程增加了Pb、Zn和Cd釋放的環(huán)境風(fēng)險(xiǎn)。力學(xué)滲透結(jié)果表明,經(jīng)過凍融的穩(wěn)定化土壤滲透系數(shù)幅度與最大值均大于未經(jīng)過穩(wěn)定化的土壤。
[Abstract]:In order to analyze the effect of freezing and thawing on the stability of heavy metals in contaminated soil, red mud and sodium sulfide were selected as additives to stabilize Pb, Zn and CD in soil. The leaching toxicity, bioavailability, soil pH and soil structure of heavy metals after freeze-thaw cycle were analyzed. The effects of freeze-thaw cycle on the long-term stability of heavy metals in stabilized soils were investigated by means of X-ray diffraction and scanning electron microscopy. The results showed that the leaching toxicity of Pb, Zn and CD in stabilized soils was higher than that of original pollution, respectively. The bioavailability of Zn and CD decreased from 28.8% and 49.5% to 11.5% and 21.8Pb from 52.9% to 57.9%. The changes of the stability of heavy metals in three soils after 60 freeze-thaw cycles were studied. The leaching toxicity of CD _ (2 +) Pb and Zn was increased by 4.27 mg / L and 89.7 mg / L compared with the stabilized samples, and the bioavailability of CD _ (2 +) Pb and Zn was slightly higher than that of the samples without freezing and thawing, with the increase of curing time and freeze-thaw time. The soil pH values showed an increasing trend. The continuous freeze-thaw cycles forced the soil voids to become larger at different stages. The results of qualitative and quantitative analysis show that the freeze-thaw process increases the environmental risk of Pb ~ (2 +) Zn and CD release. The results of mechanical permeation show that the amplitude and maximum value of soil permeability coefficient after freezing and thawing are larger than those of unstabilized soil.
【學(xué)位授予單位】:遼寧工程技術(shù)大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2015
【分類號】:X53
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