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'� -�i.=•x,t� .�.�s�r .:' #. � z a.s. d s 7 L t t''. 3-L.df.a.e'7=�rh`�1_,-.�'.`.� f�r5 � '�, .; ' ;.� � �-:.- 1�?,a:,�,^.-has z-.�4twr�i �-. _ � f'lir agTx'1��,�''.a. 't�,{7 <br /> ., .,. � ..rx,a�,. a ��.�:....... },,_•y.r?„�, .,.r t'w x,:�. ....:i�., _- - -.___�_ ��. ,n,:. ���W -..,i .,L n- ,;vr •r -F.w }�F�i�a�^1L� wf <br />� l <br /> Du Pont HLR 394-87 <br /> The progression of benzene, toluene, and xylene concentrations in the lose <br /> nutrient vessel is puzzling, in that no toluene or xylene were detected upon <br /> Initial met-up and both were detected on day 2. After day 2 the levels <br /> progressively decreased (except for 6/8/87 which follows the second addition <br /> of the throe tubstraates on 6/5/87). The three substrates decreased to <br /> undetectable levels in the medium nutrient vessel, in spite of the second <br /> addition on 6/5/87. <br /> i <br /> Discussion/Conclusifln <br /> Xylene area chosen for the CO evolution studies because it is one of the <br /> more recalcitrant materials in gaabline which is regulated for groundwater by <br /> the Environmental Protection Agency. The particular isomer employed in this <br /> study was used because no other isomers of xylene were Immediately available <br /> from commercial sources. The absence of significant differences between <br /> treatments and controls at 24, 63, or 72 hr post nutrient addition may <br /> r indicate that there was an immediate adaptation to xylene utilization and the <br /> substrate was limited upon further incubation. In addition the unlabeled <br /> xylene and ethanol used to dilute the labeled xylene may have enhanced the <br /> initial degradation. Theoretically the DPS! obtained for 4 hr should aleu be <br /> present at 24 and 72 hr. There was an apparent lose, preasum2bly by <br /> i' desorption due to saturation of the filter, of the radiolobeled CO22 from the <br /> filter, or the gradual replacement of the adsorbed labeled CD2 witg unlabeled <br /> CO2 Therefore, the assumption was anode that the greater the response at 4 <br /> hr, the more optimal the conditions for growth, hence degradation. It was <br /> difficult to determine rates of degradation using these data; therefore, the <br /> decision to scale-up on certain treatments was :Wade based upon several other <br /> pieces of information: when applying nutrient addition to the field, lower <br /> concentrations are cheaper if they provide reasonable microbial growth, and <br /> degradation; and, chemical analysis of the groundwater showed very little if <br /> any natural phosphorus and nitrogen (C. D. Litchfield 7/4/87). The three <br /> treatments which provided a response within the top 40% of treatments for <br /> both soil slurries were 5, 6, and 9. Therefore, the low nutrient and medium <br /> nutrient combinations were selected for scale-up. The top two responsive <br /> treatments from soil slurry 8-1 both contained trace metalr, while the top <br /> two responsive treatments for KW-19 did not contain trace metals. This <br /> may. <br /> suggest that depending upon the moil location, type, and contarminstSon the <br /> trace metals may or may not be available. <br /> A 6h solution of NaDH does not appear to be as good a trapping agent as <br /> AER for the groundwater from Lodi. However, because the filter did not <br /> become saturated with radiolsbeled CO2, an increase in mineralization was <br /> reflected by an increase in CO2 on the filter over seven days. This is the <br /> best situation from which to determine rates of degradation. z <br /> �� r 7 <br />