RLS898 发表于 2025-3-25 05:45:58
http://reply.papertrans.cn/23/2262/226113/226113_21.png大沟 发表于 2025-3-25 11:29:18
http://reply.papertrans.cn/23/2262/226113/226113_22.pngMOAT 发表于 2025-3-25 12:34:29
Modeling Source Zone Remediation,e physics and biogeochemistry of DNAPL source zones, more rigorous mathematical descriptions of the relationships between multiphase flow, groundwater flow, contaminant transport, mass transfer and species reactions, and superior numerical algorithms and computing power. Models are available for a w旧石器 发表于 2025-3-25 18:08:29
http://reply.papertrans.cn/23/2262/226113/226113_24.pngmanifestation 发表于 2025-3-25 22:27:36
Flux-Based Site Assessment and Management,n characterization methods and decision making. One important improvement has been the increased use of mass flux and mass discharge information. This information can be helpful for evaluating risks, assessing the benefits of partial source depletion efforts, estimating natural attenuation rates andDOSE 发表于 2025-3-26 00:16:47
Hydraulic Displacement Of Dense Nonaqueous Phase Liquids,izontal drains. This chapter focuses primarily on the application of hydraulic displacement at sites impacted by chlorinated solvent DNAPLs, although some discussion of other types of DNAPLs also is included. The chapter begins with screening calculations including examples, followed by a discussionVentilator 发表于 2025-3-26 08:11:31
http://reply.papertrans.cn/23/2262/226113/226113_27.pngDensity 发表于 2025-3-26 09:24:36
http://reply.papertrans.cn/23/2262/226113/226113_28.pngBRINK 发表于 2025-3-26 16:15:19
, Bioremediation Of Chlorinated Ethene Source Zones,ticism. However, experience over the last decade demonstrates that it is a viable technology for treating some source zones, although realistic objectives must be set. It is reasonable to expect 90-99% reductions in groundwater concentrations and mass discharge from a source in many situations, butExplosive 发表于 2025-3-26 17:05:50
Natural Attenuation Of Chlorinated Solvent Source Zones,n over time is controlled by the interaction between the rate of natural attenuation in groundwater and the rate of natural attenuation of the source. Recent advances make it possible to describe and forecast the rate of natural attenuation of the source. This information makes it possible at many s