Table 1a.
Würzburg | |||||||
W B5FH | 49°49.041′N, 9°54.955′E | Podsolige Braunerde (Cambisol) | Mixed forest (Fagus sylvatica, Carpinus betulus, Pinus sylvestris, Larix decidua) | 6.3 | 0.44 | 0.33 | 33 |
W B5FP | 49°48.960′N, 9°54.804′E | Podsolige Braunerde (Cambisol) | Mixed forest (Acer pseudoplatanus, Fagus sylvatica, Quercus robur, Pinus sylvestris) | 6.9 | 0.49 | 0.20 | 60 |
W Re4F | 49°51.540′N, 9°54.521′E | Protorendzina (Leptosol) | Deciduous forest (Carpinus betulus, Prunus sp., Quercus robur, Acer campestris) | 6.1 | 0.29 | 0.15 | 46 |
W Re1F | 49°52.553′N, 9°52.355′E | Protorendzina (Leptosol) | Mixed forest (Pinus sylvestris, Quercus petraea, Fagus sylvatica, Acer campestre) | 7.6 | 0.37 | 0.15 | 58 |
W Re3W | 49°52.234′N, 9°51.684′E | Mullartige Rendzina (Leptosol) | Meadow | 7.8 | 0.74 | 0.34 | 53 |
July 2002 | |||||||
E 5FB | 50°43.461′N, 9°47.118′E | Rendzina (Leptosol) | Mixed forest (Fagus sylvatica, Quercus sp., scattered Pinus sylvestris) | 6.5 | 1.52 | 0.21 | 177 |
MF | 51°00.000′N, 9°50.625′E | Braunerde (Cambisol) | Mixed forest (Fagus sylvatica, Quercus robur) | 4.3 | 2.62 | 1.58 | 40 |
G 15F | 51°33.974′N, 10°0.657′E | Pseudogley Parabraunerde (Gleyic Luvisol) | Deciduous forest (Fagus sylvatica, scattered Tilia platiphyllas, Acer pseudoplatanus) | 7.9 | 0.78 | 1.53 | 13 |
G 13FH | 51°31.096′N, 10°2.171′E | Rendzina (Leptosol) | Deciduous forest (Fagus sylvatica, Fraxinus excelsior, Acer platanoides) | 6.8 | 0.80 | ||
G 44F | 51°30.423′N, 10°1.167′E | Rendzina (Leptosol) | Deciduous forest (Fagus sylvatica, Fraxinus excelsior) | 7.9 | 1.80 | 1.02 | 43 |
G 44W | 51°30.411′N, 10°1.154′E | Rendzina (Leptosol) | Meadow | 8.0 | 1.38 |
Kinetic values are the maximum zero-order methane uptake rate (Vmax(app) [nanomoles of CH4 per gram of dry weight per hour]), the apparent Michaelis-Menten kinetic constant (Km(app) [ppmv of CH4]), which was calculated from Vmax(app)/a0s, and the specific affinity (a0s [milliliters of gas per gram of dry weight per hour]). a0s is a first-order rate constant. The unit milliliters refers not to milliliters of CH4 but rather to standardization to a 1-ml total gas volume. To calculate rates of atmospheric methane uptake at 25°C multiply a0s by the mixing ratio of methane in the atmosphere (1.7 ppmv of CH4 = 0.071 nmol of CH4 ml−1).
Sample was not analyzed by molecular methods.
FAO, Food and Agriculture Organization of the United Nations.