自然灾害学报
自然災害學報
자연재해학보
JOURNAL OF NATURAL DISASTERS
2009年
5期
62-69
,共8页
谢焰%谢海建%陈云敏%楼章华
謝燄%謝海建%陳雲敏%樓章華
사염%사해건%진운민%루장화
填埋场%底土%现场取样%污染物运移%理论模拟%高水头
填埋場%底土%現場取樣%汙染物運移%理論模擬%高水頭
전매장%저토%현장취양%오염물운이%이론모의%고수두
landfill%bottom soils%site sampling%contaminant transport%theoretical simulation%high water head
为了研究现场条件下污染物在粘性土中的运移机理,对运行13年的苏州七子山填埋场进行了钻孔取样.通过对土样进行分层切片、加去离子水混合并结合室内小型离心机分离,得到了填埋场底土中Cl-,Na+及COD的孔隙水浓度.将室内试验测试值和一维扩散理论进行了比较,结果表明,实测浓度剖面与扩散曲线差别较大,可见水力梯度引起的对流和机械弥散作用比分子扩散作用来得重要.将实测值与一维对流弥散解析解的计算值亦进行了比较,结果表明试验数据较为发散,但可以采用一维对流弥散理论进行大致的拟合,从而可得到运移参数的取值范围.进一步的理论预测表明,当填埋场运行30年之后,Cl-的影响深度可达到10 m以上.为了防止和延缓渗滤液污染物的进一步运移,填埋场应采取有效措施阻止渗滤液的扩散.
為瞭研究現場條件下汙染物在粘性土中的運移機理,對運行13年的囌州七子山填埋場進行瞭鑽孔取樣.通過對土樣進行分層切片、加去離子水混閤併結閤室內小型離心機分離,得到瞭填埋場底土中Cl-,Na+及COD的孔隙水濃度.將室內試驗測試值和一維擴散理論進行瞭比較,結果錶明,實測濃度剖麵與擴散麯線差彆較大,可見水力梯度引起的對流和機械瀰散作用比分子擴散作用來得重要.將實測值與一維對流瀰散解析解的計算值亦進行瞭比較,結果錶明試驗數據較為髮散,但可以採用一維對流瀰散理論進行大緻的擬閤,從而可得到運移參數的取值範圍.進一步的理論預測錶明,噹填埋場運行30年之後,Cl-的影響深度可達到10 m以上.為瞭防止和延緩滲濾液汙染物的進一步運移,填埋場應採取有效措施阻止滲濾液的擴散.
위료연구현장조건하오염물재점성토중적운이궤리,대운행13년적소주칠자산전매장진행료찬공취양.통과대토양진행분층절편、가거리자수혼합병결합실내소형리심궤분리,득도료전매장저토중Cl-,Na+급COD적공극수농도.장실내시험측시치화일유확산이론진행료비교,결과표명,실측농도부면여확산곡선차별교대,가견수력제도인기적대류화궤계미산작용비분자확산작용래득중요.장실측치여일유대류미산해석해적계산치역진행료비교,결과표명시험수거교위발산,단가이채용일유대류미산이론진행대치적의합,종이가득도운이삼수적취치범위.진일보적이론예측표명,당전매장운행30년지후,Cl-적영향심도가체도10 m이상.위료방지화연완삼려액오염물적진일보운이,전매장응채취유효조시조지삼려액적확산.
A field investigation at a 13 - year - old landfill site was carried out to study the mechanism of contaminant transport through landfill bottom soils. To assess the extent of vertical contaminant migration, continuous samples of the shallow till were obtained beneath the buried wastes and at selected locations not affected by the generated contaminants in the landfill. These samples were sectioned, and extruded pore waters were analyzed for chloride, sodium and chemical oxygen demand (COD). The field concentration profiles for chloride, sodium and COD were compared with the simulated profiles generated using a one - dimensional porous media diffusion model. The results from this comparison shows that there are large differences between the calculated curves and the filed data, indicating that advection and mechanical dispersion are clearly more important than molecular diffusion, and thus for shallow depths the soils cannot be considered as diffusion barriers. Despite the scatter of the data, the upper 4 m of the bottom soils can be approximately represented using a one - dimensional advection - dispersion approach. In calibrating the one - dimensional porous media transport model to the observed chloride profile, values for the Darcy velocity (1E-10-5E-9 m/s) , the effective diffusion coefficients and dispersive parameters for these regionally important clay deposits were obtained. The maximum migration depth of chloride was predicted to be about 10 m after 30 years of landfill operation on the basis of the obtained transport parameters. Finally, effective methods were suggested to control the successive migration of the contaminant.