Semiannual losses of nitrogen as NO and N<sub>2</sub>O from unburned and burned chaparral.
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 121, doi. 10.1029/GB003i002p00121
- By:
- Publication type:
- Article
Works matching IS 08866236 AND DT 1989 AND VI 3 AND IP 2
Results: 6
1
2
The changing patterns of ΔpCO<sub>2</sub> between ocean and atmosphere.
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 179, doi. 10.1029/GB003i002p00179
- By:
- Publication type:
- Article
3
The shallow oxygen maximum in the tropical Atlantic Ocean (Guinea Dome Area): Physical or biological origin?
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 163, doi. 10.1029/GB003i002p00163
- By:
- Publication type:
- Article
4
Ratios of dry to wet deposition of sulfur as derived from preliminary field data.
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 155, doi. 10.1029/GB003i002p00155
- By:
- Publication type:
- Article
5
Testing models of past ocean chemistry using foraminifera <sup>15</sup>N/<sup>14</sup>N.
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 107, doi. 10.1029/GB003i002p00107
- By:
- Publication type:
- Article
6
Effect of model structure on the response of terrestrial biosphere models to CO<sub>2</sub> and temperature increases.
- Published in:
- Global Biogeochemical Cycles, 1989, v. 3, n. 2, p. 137, doi. 10.1029/GB003i002p00137
- By:
- Publication type:
- Article