Structural evaluation of slow desorbing sites in model and natural solids using temperature stepped desorption profiles. 2. Column results

被引:13
作者
Castilla, HJ [1 ]
Werth, CJ [1 ]
McMillan, SA [1 ]
机构
[1] Univ Illinois, Dept Civil & Environm Engn, Urbana, IL 61801 USA
关键词
D O I
10.1021/es990430t
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Results from temperature stepped desorption (TSD) experiments are presented and compared with simulations from the TSD model presented in the first of this two-paper series. TSD columns were filled with a sand, a sediment, a soil, or a silica gel, all at 100% relative humidity. Next, TSD columns were equilibrated with trichloroethene (TCE), initially purged at 30 degrees C, and then heated to 60 degrees C after 100, 1000, or 10 000 min of slow desorption. One gamma distribution of diffusion rate constants at 30 degrees C and one gamma distribution Df diffusion rate constants at 60 degrees C were used to simulate column results at all three heating times for a single solid. At each heating time, diffusion rate constants of the gamma distributions at 30 degrees C and 60 degrees C were used to calculated an effective activation energy, E-act,E-eff. Values of E-act,E-eff for all solids were between 47 and 94 kJ/mol, on the order of activation energy values found for diffusion in microporous solids. Between 100 and 10 000 min heating times, the value of E-act,E-eff increased by a factor of 1.7 for the sand and by a factor of similar to 1.1 for the sediment and the soil. This suggests that diffusion occurs from micropores with a wider distribution of widths in the sand than in the other solids and that with decreasing mass remaining diffusion occurs from successively smaller width micropores. For the sediment, values of E-act,E-eff and (D//(2)(m)) were lower than those in the other solids. For a given sorbate, larger width micropores are associated with smaller values of E-act,E-eff and larger values of D. Hence, it is likely that micropores in the sediment are both wider and longer (i.e. larger value of /(2)(m)) than those in the other solids. These results suggest that micropore geometry varies between natural solids, and it is an important parameter that must be quantified to predict rates of slow desorption.
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页码:2966 / 2972
页数:7
相关论文
共 32 条
[1]   LONG-TERM SORPTION OF HALOGENATED ORGANIC-CHEMICALS BY AQUIFER MATERIAL .2. INTRAPARTICLE DIFFUSION [J].
BALL, WP ;
ROBERTS, PV .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1991, 25 (07) :1237-1249
[2]   MODELING THE TRANSPORT OF SOLUTES INFLUENCED BY MULTIPROCESS NONEQUILIBRIUM [J].
BRUSSEAU, ML ;
JESSUP, RE ;
RAO, PSC .
WATER RESOURCES RESEARCH, 1989, 25 (09) :1971-1988
[3]   Description of atrazine transport in soil with heterogeneous nonequilibrium sorption [J].
Chen, W ;
Wagenet, RJ .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1997, 61 (02) :360-371
[4]   DESCRIPTION OF TIME-VARYING DESORPTION-KINETICS - RELEASE OF NAPHTHALENE FROM CONTAMINATED SOILS [J].
CONNAUGHTON, DF ;
STEDINGER, JR ;
LION, LW ;
SHULER, ML .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1993, 27 (12) :2397-2403
[5]   Effects of grain-scale mass transfer on the transport of volatile organics through sediments .1. Model development [J].
Cunningham, JA ;
Werth, CJ ;
Reinhard, M ;
Roberts, PV .
WATER RESOURCES RESEARCH, 1997, 33 (12) :2713-2726
[6]   Investigation of mechanisms contributing to slow desorption of hydrophobic organic compounds from mineral solids [J].
Farrell, J ;
Grassian, D ;
Jones, M .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (08) :1237-1243
[7]   DESORPTION OF HALOGENATED ORGANICS FROM MODEL SOLIDS, SEDIMENTS, AND SOIL UNDER UNSATURATED CONDITIONS .2. KINETICS [J].
FARRELL, J ;
REINHARD, M .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1994, 28 (01) :63-72
[8]  
FARRELL J, 1993, THESIS STANFORD U
[9]   DESORPTION OF TRICHLOROETHYLENE IN AQUIFER MATERIAL - RATE LIMITATION AT THE GRAIN SCALE [J].
GRATHWOHL, P ;
REINHARD, M .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1993, 27 (12) :2360-2366
[10]  
HAGGERTY R, 1995, WATER RESOUR RES, V31, P2383, DOI 10.1029/95WR10583