Repository logo
  • English
  • 中文
Log In
Have you forgotten your password?
  1. Home
  2. College of Engineering / 工學院
  3. Environmental Engineering / 環境工程學研究所
  4. Modeling the influence of physical and chemical heterogeneity on the performance of soil remediation for organic contaminants
 
  • Details

Modeling the influence of physical and chemical heterogeneity on the performance of soil remediation for organic contaminants

Date Issued
2003-07-31
Date
2003-07-31
Author(s)
吳先琪
DOI
912211E002062
URI
http://ntur.lib.ntu.edu.tw//handle/246246/22117
Abstract
The distributed mass-transfer coefficient approach is used to model the transport of pollutants where there is heterogeneous soil texture and mass-transfer limited partition kinetics. The experimental and simulation results indicate that in a length scale larger than that of a laboratory soil column the phenomenon of non-equilibrium transport or tailing is resulted mainly from the mass-transfer limited migration of the sorbate into the stagnant region inside the immobile phases. The problem of modeling each of these immobile phases due to the lack of geological information can be improved by using a distributed mass-transfer coefficient set, which is related to some of the easily obtained soil properties such as the length scale of the system of concerned, the moisture content and the heterogeneity of the soil texture profile. Also the soil video imaging system can be used to identify and locate the layers with high hydraulic conductivity and layers with low hydraulic conductivity, or say the heterogeneity of the soil column with quite low cost and in short time, which will be a promising tool to help on the characterizing, modeling and remediation of a contaminated site. Three VOCs were used to study the interaction between humin and organic contaminants. Higher sorbing capacity of humin for more polar VOCs and the C13-NMR data of humin indicate that humin was more hydrophilic than Aldrich humic acid. The apparent diffusivity of acetone, toluene, and hexane in the disks ranged from 10-8 to 10-10 cm2/s. The sorbed toluene in humin does not seem persistent to desorption; however, acetone and hexane, either a polar or a linear compound, show persistence against desorption. On the completion of the desorption experiments, there were approximately 35% and 20% sorbate residue for acetone and hexane, respectively. The sorption kinetics of toluene in dry and humid clay films was investigated by tracking the change of the IR absorbance. Under humid condition, similar toluene sorbed intensities are found on Ca -and Cu– montmorillonites. However, higher intensities of toluene sorbed were found on Cu-form under dry condition, which indicates stronger interaction occurring. On Ca- and Cu-montmorillonite, some portion of toluene is desorbed at an extremely slow rate under dry conditions. Either some original toluene peaks or some new peaks are persistent against desorption from montmorillonites, also suggesting the existence of irreversibly sorbed species. Theremay be some transformation of VOCs in clay systems. Although the persistence was not observed under high humidity conditions by spectroscopic method, the clay minerals could be a controlling factor of slow desorption in soil. The sorption and desorption of trichloroethylene (TCE) in humic acid and humin disks was investigated by microbalance. The apparent diffusivity of TCE in these two humic substances was in the 10-8 to 10-9 cm2/s magnitude. There are no residual sorbed TCE observed via a microbalance. The intrinsic sorption/desorption time scale of TCE on two cation exchanged montmorillonites was only few minutes by thin film/FTIR method. Molecular dynamic simulations were also used to study the sorption of organic contaminants in soil organic matter. The simulation results of the sorption kinetics and thermodynamics of toluene in humic acid are in good agreement with the experimental data. We believe that this technique will become a powerful tool not only to facilitate the solving of the problems of contaminated soil clean-up but also to be applied to a wider range of environmental problems. After studying soil chemical heterogeneity, we found the intrinsic sorption is fast for VOCs into humin, humic acid, and montmorillonite. So they do not contribute to the sequestration process in soils. The mass transfer of contaminants into soil plays the important role on the slow sorption/desorption in soils.
Subjects
不均質性
SDGs

[SDGs]SDG11

Publisher
臺北市:國立臺灣大學環境工程學研究所
Type
report
File(s)
Loading...
Thumbnail Image
Name

912211E002062.pdf

Size

2.49 MB

Format

Adobe PDF

Checksum

(MD5):6d6351cc6c400f9573eeedc081ed78c5

臺大位居世界頂尖大學之列,為永久珍藏及向國際展現本校豐碩的研究成果及學術能量,圖書館整合機構典藏(NTUR)與學術庫(AH)不同功能平台,成為臺大學術典藏NTU scholars。期能整合研究能量、促進交流合作、保存學術產出、推廣研究成果。

To permanently archive and promote researcher profiles and scholarly works, Library integrates the services of “NTU Repository” with “Academic Hub” to form NTU Scholars.

總館學科館員 (Main Library)
醫學圖書館學科館員 (Medical Library)
社會科學院辜振甫紀念圖書館學科館員 (Social Sciences Library)

開放取用是從使用者角度提升資訊取用性的社會運動,應用在學術研究上是透過將研究著作公開供使用者自由取閱,以促進學術傳播及因應期刊訂購費用逐年攀升。同時可加速研究發展、提升研究影響力,NTU Scholars即為本校的開放取用典藏(OA Archive)平台。(點選深入了解OA)

  • 請確認所上傳的全文是原創的內容,若該文件包含部分內容的版權非匯入者所有,或由第三方贊助與合作完成,請確認該版權所有者及第三方同意提供此授權。
    Please represent that the submission is your original work, and that you have the right to grant the rights to upload.
  • 若欲上傳已出版的全文電子檔,可使用Open policy finder網站查詢,以確認出版單位之版權政策。
    Please use Open policy finder to find a summary of permissions that are normally given as part of each publisher's copyright transfer agreement.
  • 網站簡介 (Quickstart Guide)
  • 使用手冊 (Instruction Manual)
  • 線上預約服務 (Booking Service)
  • 方案一:臺灣大學計算機中心帳號登入
    (With C&INC Email Account)
  • 方案二:ORCID帳號登入 (With ORCID)
  • 方案一:定期更新ORCID者,以ID匯入 (Search for identifier (ORCID))
  • 方案二:自行建檔 (Default mode Submission)
  • 方案三:學科館員協助匯入 (Email worklist to subject librarians)

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science