Existing alternative tests to measure side‐effects of pesticides on soil microorganisms: Dehydrogenase activity

1991 ◽  
Vol 30 (3-4) ◽  
pp. 167-176 ◽  
Author(s):  
H.‐P. Malkomes
1985 ◽  
Vol 20 (5) ◽  
pp. 457-488 ◽  
Author(s):  
L. Zelles ◽  
I. Scheunert ◽  
F. Korte

2021 ◽  
Vol 26 (3) ◽  
pp. e2219
Author(s):  
Helena Dvorackova ◽  
Jaroslav Záhora ◽  
Lubica Pospíšilová ◽  
Vítězslav Vlček

Objective. Dehydrogenase activity after the biological activation of biochar by the native soil microorganisms was studied. The main aim was to improve biochar properties by activation and make it more friendly for the soil microflora. Materials and methods. The activation was reached by aerating with the soil solution for two weeks. No special inoculum of microorganisms was applied. The following treatments in four replicates were prepared: conventional raw biochar (BR), activated biochar (BA), mineral fertilizer DAM 390 (NF), and control (C). A statistical test for comparing treatments means (Fisher p≤0.05; program STATISTICA 12.0; StatSoft software Inc., Tulsa, Oklahoma, USA) was used. Results. Statistically significant differences in the dehydrogenase activity between the treatments BR, BA, and C were found. Application of mineral fertilizers had a negative effect and increasing of nitrogen leaching was observed. Conclusions. Activating of biochar is suitable metods for impove soil biota conition compared with convention biochar.


2003 ◽  
Vol 38 (11) ◽  
pp. 1329-1335 ◽  
Author(s):  
Mara Mercedes de Andréa ◽  
Terezinha Bonanho Peres ◽  
Luiz Carlos Luchini ◽  
Sheila Bazarin ◽  
Solange Papini ◽  
...  

Pesticide degradation studies are essential to evaluate its impact in the environment and on non-target organisms. The effect of repeated soil applications of the herbicide glyphosate on its dissipation and on soil microorganisms was studied by radiometric and microbial techniques. Results indicated fast dissipation of the [14C]-glyphosate or [14C]metabolites extractable residues (half-life of 0.92±0.29 month), but increasing half-lives of total mineralization ranging from 2.2 to 3.4 months as the number of applications increased from 1 to 4. No significant correlation was found between 14CO2 production and dehydrogenase activity.


2008 ◽  
Vol 38 (2) ◽  
pp. 161-167 ◽  
Author(s):  
Raktim Pal ◽  
Piw Das ◽  
Kalyan Chakrabarti ◽  
Ashis Chakraborty ◽  
Ashim Chowdhury

2002 ◽  
Vol 68 (4) ◽  
pp. 1808-1816 ◽  
Author(s):  
Ulla C. Brinch ◽  
Flemming Ekelund ◽  
Carsten S. Jacobsen

ABSTRACT We examined the harmful side effects on indigenous soil microorganisms of two organic solvents, acetone and dichloromethane, that are normally used for spiking of soil with polycyclic aromatic hydrocarbons for experimental purposes. The solvents were applied in two contamination protocols to either the whole soil sample or 25% of the soil volume, which was subsequently mixed with 75% untreated soil. For dichloromethane, we included a third protocol, which involved application to 80% of the soil volume with or without phenanthrene and introduction of Pseudomonas fluorescens VKI171 SJ132 genetically tagged with luxAB::Tn5. For both solvents, application to the whole sample resulted in severe side effects on both indigenous protozoa and bacteria. Application of dichloromethane to the whole soil volume immediately reduced the number of protozoa to below the detection limit. In one of the soils, the protozoan population was able to recover to the initial level within 2 weeks, in terms of numbers of protozoa; protozoan diversity, however, remained low. In soil spiked with dichloromethane with or without phenanthrene, the introduced P. fluorescens VKI171 SJ132 was able to grow to a density 1,000-fold higher than in control soil, probably due mainly to release of predation from indigenous protozoa. In order to minimize solvent effects on indigenous soil microorganisms when spiking native soil samples with compounds having a low water solubility, we propose a common protocol in which the contaminant dissolved in acetone is added to 25% of the soil sample, followed by evaporation of the solvent and mixing with the remaining 75% of the soil sample.


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