scholarly journals Methodological Modifications for Accurate and Efficient Determination of Contaminant Biodegradation in Unsaturated Calcareous Soils

1991 ◽  
Vol 57 (3) ◽  
pp. 717-720 ◽  
Author(s):  
Mary E. Watwood ◽  
Carleton S. White ◽  
Clifford N. Dahm
Keyword(s):  
1989 ◽  
Vol 69 (2) ◽  
pp. 191-197
Author(s):  
W. VAN LIEROP

The objective of this study was to determine the effect of adding either 0.001M EDTA or 0.005M DTPA on the amount of P removed from acid and calcareous soils by the Kelowna and 0.25M HO Ac extractants. These complexing agents were studied for possible simultaneous extraction and determination of available Zn. To achieve that end, P-concentrations removed by these solutions from a group of acid, calcareous, and combined soils were compared against reference values obtained with 0.5M NaHCO3 (Olsen et al.) and the Kelowna extractant (0.25M HOAc + 0.015M NH4F) by means of graphing, correlation and regression techniques. Of the 80 soils studied, 40 were acid with pH (H2O) values ranging from 4.2 to 6.9 and the remainder having higher values up to 9.3. Results indicated that additions of either 0.001M EDTA or 0.005M DTPA to the Kelowna solution increased average extracted P concentrations by about 20 and 60%, respectively. Values removed by either of the new KEDTA and KDTPA solutions were closely related to those extracted with 0.5M NaHCO3 and Kelowna solutions on acid and calcareous soils (r values ≥ 0.96**). As EDTA and DTPA increased extracted soil P, these were added at 0.001 and 0.005M as NH4 preparations to 0.25M HOAc (AADTPA & AAEDTA; without fluoride), respectively, for determining whether these complexing agents could supplant F for P extraction. These solutions removed proportionally related amounts (r ≈ 0.94**) of P from calcareous, compared to the Kelowna and 0.5M NaHCO3 solutions, but relationships were less precise for acid soils (r ≈ 0.76**). These results suggest that the AADTPA or AAEDTA solution should be evaluated further before adoption for routine P determination in multiple element extractions. Key words: Mehlich in, acid soils, calcareous soils


1962 ◽  
Vol 10 (3) ◽  
pp. 217-222 ◽  
Author(s):  
D.H. Yaalon ◽  
J. Van Schuylenborgh ◽  
S. Slager

The soil is saturated with LiCl solution buffered at pH 8.2 with LiOAc, followed immediately by leaching with Ca(OAc)2 at pH 8.2. Na, K, Ca, Mg and Li are determined in the extracts by direct flame photometry and complexometry. The need for washing the soil is eliminated by assaying the remaining excess salts as C1. Soluble ions are determined on a separate sample. The method can be used on non-saline or CO3-free soils by adjusting the saturating and extracting solutions to pH 7. (Abstract retrieved from CAB Abstracts by CABI’s permission)


2021 ◽  
Vol 52 (19) ◽  
pp. 2207-2216
Author(s):  
Fatma Gokmen Yilmaz ◽  
Aysegul Korkmaz ◽  
Yusuf Isik ◽  
Nazlı Can Saglik ◽  
Duygu Akcay Kulluk ◽  
...  
Keyword(s):  

1999 ◽  
Vol 79 (4) ◽  
pp. 529-533 ◽  
Author(s):  
R. L. Haney ◽  
A. J. Franzluebbers ◽  
F. M. Hons ◽  
D. A. Zuberer

Routine determination of soil microbial biomass C has shifted during the past decade from chloroform fumigation-incubation to chloroform fumigation-extraction using 0.5 M K2SO4 as extractant. We compared extractable C with water and 0.5 M K2SO4 in eight soils ranging in pH from 5.4 to 8.3. In unfumigated soils with low pH, extractable C was 0.8- to 1.2-fold greater with water than with 0.5 M K2SO4. However, in unfumigated soils with pH > 7.7, extractable C, although not statistically significant, was 11 to 19% less with water than with 0.5 M K2SO4. In fumigated soils, no difference in extractable C between water and 0.5 M K2SO4 was detected among soils with pH < 7.7, but extractable C was 13 to 17% less with water than with 0.5 M K2SO4 with pH > 7.7. Our results suggest that 0.5 M K2SO4 (1) may flocculate soil and cause adsorption of solubilized C onto colloids at pH < 7.7, but (2) may disperse calcareous soils at pH > 7.7, thereby differentially affecting the fate of solubilized C depending upon soil pH. Our results put into question the widespread adaptability of using chloroform fumigation-extraction to estimate microbial biomass C. Key words: Extractable carbon, chloroform fumigation-extraction, microbial biomass


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