找回密碼
 To register

QQ登錄

只需一步,快速開始

掃一掃,訪問微社區(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

[復制鏈接]
樓主: 縮寫
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).
 關于派博傳思  派博傳思旗下網站  友情鏈接
派博傳思介紹 公司地理位置 論文服務流程 影響因子官網 吾愛論文網 大講堂 北京大學 Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點評 投稿經驗總結 SCIENCEGARD IMPACTFACTOR 派博系數 清華大學 Yale Uni. Stanford Uni.
QQ|Archiver|手機版|小黑屋| 派博傳思國際 ( 京公網安備110108008328) GMT+8, 2025-10-25 00:48
Copyright © 2001-2015 派博傳思   京公網安備110108008328 版權所有 All rights reserved
快速回復 返回頂部 返回列表
九龙城区| 榆树市| 大石桥市| 托克逊县| 鄢陵县| 永德县| 高安市| 大化| 赤壁市| 五大连池市| 梧州市| 潜江市| 冀州市| 理塘县| 正蓝旗| 巴塘县| 游戏| 浑源县| 汉川市| 扬州市| 宾阳县| 柳林县| 潜江市| 八宿县| 汤原县| 龙州县| 武川县| 伊春市| 望谟县| 英超| 阳曲县| 龙岩市| 韩城市| 秀山| 吴桥县| 苏尼特右旗| 美姑县| 福泉市| 喀什市| 扶沟县| 靖西县|