| nr |
titel |
auteur |
tijdschrift |
jaar |
jaarg. |
afl. |
pagina('s) |
type |
| 1 |
A new technique for determining equilibrium hydrogen isotope fractionation factors using the ion microprobe: application to the epidote-water system
|
Chacko, Thomas
|
|
1999
|
63 |
1 |
p. 1-10
10 p.
|
artikel
|
| 2 |
Carbon isotopic fractionation in lipids from methanotrophic bacteria II: the effects of physiology and environmental parameters on the biosynthesis and isotopic signatures of biomarkers
|
Jahnke, Linda L
|
|
1999
|
63 |
1 |
p. 79-93
15 p.
|
artikel
|
| 3 |
Coupled anoxic nitrification/manganese reduction in marine sediments
|
Hulth, Stefan
|
|
1999
|
63 |
1 |
p. 49-66
18 p.
|
artikel
|
| 4 |
Identification of novel sulfur-containing steroids in sediments and petroleum: probable incorporation of sulfur into δ5,7-sterols during early diagenesis
|
Sinninghe Damsté, Jaap S
|
|
1999
|
63 |
1 |
p. 31-38
8 p.
|
artikel
|
| 5 |
Influence of sorbate-sorbent interactions on the crystallization kinetics of nickel- and lead-ferrihydrite coprecipitates
|
Ford, Robert G.
|
|
1999
|
63 |
1 |
p. 39-48
10 p.
|
artikel
|
| 6 |
Origin of middle rare earth element enrichments in acid waters of a Canadian High Arctic lake
|
Johannesson, Kevin H
|
|
1999
|
63 |
1 |
p. 153-165
13 p.
|
artikel
|
| 7 |
Radioisotope tracer studies of inorganic carbon and Ca in microbially derived CaCO3
|
Yates, Kimberly K
|
|
1999
|
63 |
1 |
p. 129-136
8 p.
|
artikel
|
| 8 |
Redox zoning, rates of sulfate reduction and interactions with Fe-reduction and methanogenesis in a shallow sandy aquifer, Rømø, Denmark
|
Jakobsen, Rasmus
|
|
1999
|
63 |
1 |
p. 137-151
15 p.
|
artikel
|
| 9 |
Scavenging of dissolved yttrium and rare earths by precipitating iron oxyhydroxide: experimental evidence for Ce oxidation, Y-Ho fractionation, and lanthanide tetrad effect
|
Bau, Michael
|
|
1999
|
63 |
1 |
p. 67-77
11 p.
|
artikel
|
| 10 |
Structure and properties of magmatic liquids: from haplobasalt to haploandesite1 1 In the Qi-notation, a superscript, i, is used to denote the number of bridging oxygens (equal to 4- number of nonbridging oxygen) in the species. Therefore, Q4 as 4 bridging and 0 nonbridging oxygen (NBO/Si = 0). Q3 has 3 bridging and 1 nonbridging oxygen (NBO/Si = 1), Q2 has 2 bridging and 2 nonbridging oxygen (NBO(/Si = 2), Q1 has 1 bridging and 3 nonbridging oxygen (NBO/Si = 3), and Q0 has 0 bridging and 4 nonbridging oxygen (NBO/Si = 4).
|
Mysen, Bjorn O.
|
|
1999
|
63 |
1 |
p. 95-112
18 p.
|
artikel
|
| 11 |
The hydrosulphide/sulphide complexes of copper(I): experimental determination of stoichiometry and stability at 22°c and reassessment of high temperature data
|
Mountain, B.W.
|
|
1999
|
63 |
1 |
p. 11-29
19 p.
|
artikel
|
| 12 |
The influence of size distribution on the particle concentration effect and trace metal partitioning in rivers
|
Benoit, Gaboury
|
|
1999
|
63 |
1 |
p. 113-127
15 p.
|
artikel
|
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