截断
发表于 2025-3-23 11:39:40
http://reply.papertrans.cn/28/2791/279041/279041_11.png
MEET
发表于 2025-3-23 15:32:45
,Risk Assessment — Remediation,time scales are discussed, together with desorption processes desorption processes, limiting aquifer and soil remediation. Finally a comparison of advective and diffusive solute transport is provided.
Bereavement
发表于 2025-3-23 18:31:45
http://reply.papertrans.cn/28/2791/279041/279041_13.png
Debark
发表于 2025-3-24 02:12:57
http://reply.papertrans.cn/28/2791/279041/279041_14.png
法律的瑕疵
发表于 2025-3-24 02:37:44
http://reply.papertrans.cn/28/2791/279041/279041_15.png
FATAL
发表于 2025-3-24 10:04:32
Liberalism and Practical Reasonusive mass transfer phenomena. Methods for the calculation of diffusion coefficients in vapor and aqueous phase are introduced and the definition of diffusion coefficients in porous media for steady state and transient conditions is given. Surface diffusion and diffusion in natural organic matter (p
Limpid
发表于 2025-3-24 12:34:03
http://reply.papertrans.cn/28/2791/279041/279041_17.png
千篇一律
发表于 2025-3-24 17:57:40
Tourism, Development, and Sustainabilityanglia. The following chapter addresses the mass transfer processes which control the release of organic compounds from NAPLs and multicomponent NAPL mixtures such as coal tar or creosote. The mass transfer into the aqueous phase depends on the compound’s water solubility and molecular diffusivity.
贪心
发表于 2025-3-24 21:04:14
Environmental Challenges and Solutionsmass transfer zones is briefly introduced which can be used for risk assessment, e.g. to distinguish maximum contaminant concentrations (equilibrium, e.g. dissolution from residual phase) from maximum contaminant flux (non-equilibrium, e.g. due to slow desorption) into groundwater. Transport of vola
tangle
发表于 2025-3-25 02:55:32
Reification and Empty AbstractionThis chapter provides methods for the calculation of diffusion rates for various boundary conditions in porous particles and low permeability sediment layers. Emphasis is placed on the modeling of sorption/desorption kinetics (including heterogeneous aquifer materials) and diffusion across low permeability layers (e.g. mineral liners).