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. Author manuscript; available in PMC: 2014 Jan 15.
Published in final edited form as: Water Res. 2012 Sep 18;46(19):6454–6462. doi: 10.1016/j.watres.2012.09.020

Table 2.

Properties of aquifer materials. Surface area was measured in our laboratory while the other properties were analyzed by the Analytical Laboratory at the University of California, Davis. Details on the analytical protocols are available at http://anlab.ucdavis.edu/analyses/soil/

Soil ID Sand (wt. %) Silt (wt. %) Clay (wt. %) pH pHava BET surface areab (m2/g) Total Fe (mg/kg) Total Mn (mg/kg) Fe-CBD (mg/kg) Mn-CBD (mg/kg) TC (%) TOC (%)
CADIR 80 16 4 8.4 8.4 4.7 9600 96 2460 28 0.22 0.1
CADOU 84 10 6 9.2 8.7 3.9 7700 106 3020 54 0.32 0.2
CADMS 90 5 5 8.8 8.5 3.2 6840 90 2400 44 0.23 0.11
CAROL 63 18 19 7.6 8.2 39.8 24880 156 4800 76 0.08 0.08
AWBPH 82 10 8 7.8 8.5 14.3 16700 287 8010 191 0.03* 0.04*
AFTCS 60 22 18 7.7 8.3 27.7 14400 321 4470 185 0.36 0.05
AMTAL 64 22 14 7.2 8.2 16.2 18490 1162 10500 943 0.04* 0.06*
WYSAN 86 8 6 7.8 8.5 9.0 11500 193 4170 142 0.19 0.04
WYLAM 42 32 26 7.7 8.3 34.6 13900 294 2580 189 0.34 0.04
KENTK 87 5 8 4.6 7.2 5.1 12400 67 10950 57 0.02* 0.05*
*

TOC (Total Organic Carbon) was greater than TC (Total Carbon) because these values were within the uncertainty range of the analysis methods.

a

The average pH of the solution during the course of phenol degradation experiment. Solutions were buffered with 10 mM borate and the initial pH was 8.5.

b

BET surface area was measured in duplicate, and the average results are reported.