找回密碼
 To register

QQ登錄

只需一步,快速開(kāi)始

掃一掃,訪問(wèn)微社區(qū)

打印 上一主題 下一主題

Titlebook: Diffusion in Natural Porous Media; Contaminant Transpor Peter Grathwohl Book 1998 Springer Science+Business Media New York 1998 Contaminati

[復(fù)制鏈接]
樓主: 縮寫(xiě)
11#
發(fā)表于 2025-3-23 11:39:40 | 只看該作者
12#
發(fā)表于 2025-3-23 15:32:45 | 只看該作者
,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.
13#
發(fā)表于 2025-3-23 18:31:45 | 只看該作者
14#
發(fā)表于 2025-3-24 02:12:57 | 只看該作者
15#
發(fā)表于 2025-3-24 02:37:44 | 只看該作者
16#
發(fā)表于 2025-3-24 10:04:32 | 只看該作者
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
17#
發(fā)表于 2025-3-24 12:34:03 | 只看該作者
18#
發(fā)表于 2025-3-24 17:57:40 | 只看該作者
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.
19#
發(fā)表于 2025-3-24 21:04:14 | 只看該作者
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
20#
發(fā)表于 2025-3-25 02:55:32 | 只看該作者
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).
 關(guān)于派博傳思  派博傳思旗下網(wǎng)站  友情鏈接
派博傳思介紹 公司地理位置 論文服務(wù)流程 影響因子官網(wǎng) 吾愛(ài)論文網(wǎng) 大講堂 北京大學(xué) Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點(diǎn)評(píng) 投稿經(jīng)驗(yàn)總結(jié) SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學(xué) Yale Uni. Stanford Uni.
QQ|Archiver|手機(jī)版|小黑屋| 派博傳思國(guó)際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-25 13:11
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved
快速回復(fù) 返回頂部 返回列表
兰州市| 西峡县| 南宁市| 东源县| 曲靖市| 天柱县| 上高县| 恩平市| 宜都市| 右玉县| 手游| 彭州市| 越西县| 郁南县| 奉化市| 六盘水市| 四川省| 阿拉善右旗| 察哈| 高州市| 靖州| 铅山县| 紫阳县| 鄄城县| 彝良县| 阿巴嘎旗| 疏附县| 郧西县| 昌宁县| 武强县| 利川市| 边坝县| 威海市| 汾阳市| 凯里市| 蕉岭县| 黄陵县| 鄄城县| 油尖旺区| 翼城县| 饶平县|