Physical Determinants of Methane Oxidation Capacity in a Temperate Soil

Methane oxidation capacity of soil from an experimentalsite in Northwest England was strongly dependent on temperatureand percentage water holding capacity. The soil had a distincttemperature optimum of 25 °C, with capacity for net methaneoxidation being completely lost below 5 and greater than37 °C. Optimum percentage water holding capacity for methaneoxidation was in the range 30–60%, with significant reductions inmethane oxidation rates in soils outside this range. Organic andmineral layers within the soil showed differences in potentialmethane oxidation rate, with methane oxidation being most rapid inthe buried organic layer and least rapid in the surface organiclayer. The importance of soil structure and gas diffusionlimitation is underlined, as is the strong temperature dependenceof methane oxidation when such diffusion limitation is removed.     

Nitrous oxide emission from some English and Welsh rivers and estuaries

Nutrient and N₂O concentrations in the water columns were measured seasonally over a full salinity range in the nutrified rivers Colne, Stour, Orwell, Deben, Trent, Ouse and Humber and their estuaries on the east coast of England between August 2001 and May 2002, and in the oligotrophic rivers Conwy, Dovey and Mawddach in North and West Wales between August 2002 and May 2003. Nutrient and N₂O concentrations in the nutrified English rivers and estuaries were much higher than those in the Welsh rivers. N₂O concentrations and % saturation in the estuaries were significantly correlated with nitrate, nitrite and ammonium concentrations in the water. The strongest correlation was with nitrite (r ² = 0.56, p < 0.01), suggesting that nitrite was the most significant factor among the different nutrients in regulating N₂O concentration in the estuaries. N₂O concentrations in the English rivers and estuaries were supersaturated throughout the year with annual averages from 186.9 to 992.9%, indicating that these rivers and estuaries were sources of atmospheric N₂O, whereas in the Welsh rivers N₂O concentrations were much lower with annual averages from 113.6 to 137.4% saturation. Although the estuarine area in the Colne was almost the same as that in the Conwy, the annual N₂O emission from the Colne was much higher (937498 mol N yr^?1) than in the Conwy (23020 mol N yr^?1). On the east coast, riverine emissions of N₂O were only 0.5–12.5% of the total emission from rivers and estuaries. Thus rivers were negligible, but estuaries were significant contributors to the UK N₂O inventory.     

Temperature-induced changes in the formation of sulphide in a marine sediment

The influence of temperature upon sulphide formation was investigated with sediment sulphureta incubated at constant temperatures in the laboratory. The concentrations of sulphate, sulphide and pyrite were periodically measured and it was found that, in addition to a decrease in the rate of sulphide formation with temperature, there was a changes in the origin of the sulphide. Thus, at 5° and 10°C, the majority of sulphide originated from organic sulphur, while sulphate contributed the greater proportion of the sulphide at 20° and 30°C. Such changes presumably reflect those in the natural enviroment during winter and summer.     

Nitrous oxide emission from some English and Welsh rivers and estuaries

Nutrient and N₂O concentrations in the water columns were measured seasonally over a full salinity range in the nutrified rivers Colne, Stour, Orwell, Deben, Trent, Ouse and Humber and their estuaries on the east coast of England between August 2001 and May 2002, and in the oligotrophic rivers Conwy, Dovey and Mawddach in North and West Wales between August 2002 and May 2003. Nutrient and N₂O concentrations in the nutrified English rivers and estuaries were much higher than those in the Welsh rivers. N₂O concentrations and % saturation in the estuaries were significantly correlated with nitrate, nitrite and ammonium concentrations in the water. The strongest correlation was with nitrite (r² = 0.56, p < 0.01), suggesting that nitrite was the most significant factor among the different nutrients in regulating N₂O concentration in the estuaries. N₂O concentrations in the English rivers and estuaries were supersaturated throughout the year with annual averages from 186.9 to 992.9%, indicating that these rivers and estuaries were sources of atmospheric N₂O, whereas in the Welsh rivers N₂O concentrations were much lower with annual averages from 113.6 to 137.4% saturation. Although the estuarine area in the Colne was almost the same as that in the Conwy, the annual N₂O emission from the Colne was much higher (937498 mol N yr^–1) than in the Conwy (23020 mol N yr^–1). On the east coast, riverine emissions of N₂O were only 0.5–12.5% of the total emission from rivers and estuaries. Thus rivers were negligible, but estuaries were significant contributors to the UK N₂O inventory.     

The effect of microbial activity upon the sedimentary sulphur cycle

The sulphate content of an intertidal sediment at Anglesey (UK) was shown to vary during the year, the sulphate-reducing activity of the microbial population being limited by low temperature during winter, and by the low numbers of sulphate-reducing bacteria during May, 1969. A corresponding annual variation of the sedimentary sulphide could not be demonstrated, and the sulphide which was formed biologically during the course of the year was almost entirely lost from the sediment. This loss of sulphide was probably due to subsurface oxidation; and flushing, by water entering at the base of the sediment. It is suggested that sulphide was only precipitated within the sediment during summer when sulphate reduction was active, and even then only during part of the tidal cycle when flushing did not occur.     

The seasonal selection by temperature of heterotrophic bacteria in an intertidal sediment

The seasonal selection by temperature of bacteria in an intertidal sediment was investigated, and a simplified method of demonstrating the temperature adaption of a mixed heterotrophic bacterial population was suggested. The method relied upon counting the bacteria which grew at only two separate incubation-temperatures, and compared favourably with more tedions methods which utilise replicated cultures grown at a large number of incubation temperatures. Using this technique, a temperature adaptation index was calculated for the heterotrophic bacterial population and changes in the value of this index were shown to be correlated with seasonal changes of environmental temperature.