Pattern of elemental release during the granite dissolution can be changed by aerobic heterotrophic bacterial strains isolated from Damma Glacier (central Alps) deglaciated granite sand.
about
Hydrogen Cyanide in the Rhizosphere: Not Suppressing Plant Pathogens, but Rather Regulating Availability of PhosphateVariations in soil culturable bacteria communities and biochemical characteristics in the Dongkemadi glacier forefield along a chronosequence.Correlation of the abundance of betaproteobacteria on mineral surfaces with mineral weathering in forest soilsDiversity, resistance and resilience of the bacterial communities at two alpine glacier forefields after a reciprocal soil transplantation.Mineral Types and Tree Species Determine the Functional and Taxonomic Structures of Forest Soil Bacterial Communities.Isolation and the interaction between a mineral-weathering Rhizobium tropici Q34 and silicate minerals.Tales from the tomb: the microbial ecology of exposed rock surfaces.Location-Related Differences in Weathering Behaviors and Populations of Culturable Rock-Weathering Bacteria Along a Hillside of a Rock Mountain.Identification of biomass utilizing bacteria in a carbon-depleted glacier forefield soil by the use of 13C DNA stable isotope probing.Variations in culturable bacterial communities and biochemical properties in the foreland of the retreating Tianshan No. 1 glacierLaboratory Tools to Quantify Biogenic Dissolution of Rocks and Minerals: A Model Rock Biofilm Growing in Percolation Columns
P2860
Q28821183-22D7F2C2-F76B-4E9A-B3FD-8321BC963A36Q34276490-82E95D04-E445-4BE7-9A67-1B9C69CBBBADQ34338242-9FFCA718-505A-4D3B-A3E4-12623E9752FEQ35103277-7BAE143B-9732-4383-8CD3-29769B8717FFQ39076958-E76641CF-3DDF-4C50-861E-F401DCDC37C6Q45694054-D763BFB6-BF94-40DC-A058-D7CB22928E6DQ46242290-44973138-83B9-4BD7-9880-900721D239ACQ46441886-0738FF12-903E-4B46-A8DF-3FF9DCFCDE08Q50479194-DBA31687-9B2C-46A3-A825-5BB313C6CEBEQ56889919-E40BBA07-5AE3-4024-B6E8-DB295FAA19D0Q57896810-35E77AA7-B048-4087-AB7C-FCE966B38425
P2860
Pattern of elemental release during the granite dissolution can be changed by aerobic heterotrophic bacterial strains isolated from Damma Glacier (central Alps) deglaciated granite sand.
description
2011 nî lūn-bûn
@nan
2011 թուականի Նոյեմբերին հրատարակուած գիտական յօդուած
@hyw
2011 թվականի նոյեմբերին հրատարակված գիտական հոդված
@hy
2011年の論文
@ja
2011年論文
@yue
2011年論文
@zh-hant
2011年論文
@zh-hk
2011年論文
@zh-mo
2011年論文
@zh-tw
2011年论文
@wuu
name
Pattern of elemental release d ...... lps) deglaciated granite sand.
@ast
Pattern of elemental release d ...... lps) deglaciated granite sand.
@en
Pattern of elemental release d ...... ns isolated from Damma Glacier
@nl
type
label
Pattern of elemental release d ...... lps) deglaciated granite sand.
@ast
Pattern of elemental release d ...... lps) deglaciated granite sand.
@en
Pattern of elemental release d ...... ns isolated from Damma Glacier
@nl
prefLabel
Pattern of elemental release d ...... lps) deglaciated granite sand.
@ast
Pattern of elemental release d ...... lps) deglaciated granite sand.
@en
Pattern of elemental release d ...... ns isolated from Damma Glacier
@nl
P2093
P2860
P1433
P1476
Pattern of elemental release d ...... lps) deglaciated granite sand.
@en
P2093
Aleš Lapanje
Celine Wimmersberger
Gerhard Furrer
Ivano Brunner
P2860
P2888
P304
P356
10.1007/S00248-011-9976-7
P577
2011-11-22T00:00:00Z
P6179
1052437233