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pro vyhledávání: '"Richard G. Burns"'
Autor:
Richard G. Burns, Caroline S. Young
Publikováno v:
Soil Biochemistry ISBN: 9781003208884
Soil Biochemistry
Soil Biochemistry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98013ead39cc2f4fbdf8cfee77dcf355
https://doi.org/10.1201/9781003208884-1
https://doi.org/10.1201/9781003208884-1
Autor:
Richard G. Burns
Publikováno v:
Soil Biology and Biochemistry. 147:107818
Survival in Sterile Soil and Atrazine Degradation ofPseudomonassp. Strain ADP Immobilized on Zeolite
Publikováno v:
Bioremediation Journal. 18:309-316
In laboratory settings, the ability of bacteria and fungi to degrade many environmental contaminants is well proven. However, the potential of microbial inoculants in soil remediation has not often been realized because catabolically competent strain
Autor:
Richard G. Burns
Publikováno v:
Soil Biology and Biochemistry. 123:A1-A2
Publikováno v:
Applied Clay Science. 64:90-93
Storage and delivery of beneficial microorganisms are fundamental issues determining their value and effectiveness for a wide range of industrial and environmental purposes. One such application is the use of bacteria for the remediation of soil poll
Autor:
Richard G. Burns
Publikováno v:
Soil Biology and Biochemistry. 105:A1-A2
Publikováno v:
Plant and Soil. 348:269-279
Soils are frequently exposed to drying and wetting events and previous studies have shown that rewetting results in a strong but short-lived flush of microbial activity. The aim of this study was to determine the effect of the water content during th
Soil microbial activity and community composition: Impact of changes in matric and osmotic potential
Publikováno v:
Soil Biology and Biochemistry. 43:1229-1236
As saline soils dry, the salt in the remaining solution phase is concentrated and the microbes are subjected to both water and osmotic stress. However, little is known about the interactive effect of matric potential (MP) and osmotic potential (OP) o
Publikováno v:
Plant and Soil. 344:241-254
Low soil water content (low matric potential) and salinity (low osmotic potential) occur frequently in soils, particularly in arid and semi-arid regions. Although the effect of low matric or low osmotic potential on soil microorganisms have been stud
Autor:
Richard G. Burns
Publikováno v:
Soil Biology and Biochemistry. 68:A1-A3