Torbert HA, Wood CW (1992) Effects of soil compaction and water-filled pore space on soil microbial activity and N losses. Commun Soil Sci Plan 23:1321–1331. : 10.1080/00103629209368668Torbert, H. A. & Wood, C. W. 1992 . Effects of soil compaction and waterfilled pore ...
autotrophic nitrification and heterotrophic nitrification in a fertilised (200 kg N ha−1) silt loam soil at contrasting (20–70%) water-filled pore space (WFPS).15N-N2O emissions from14NH415NO3replicates were attributed
Our results derived from IR experiments and MD simulations strongly suggest that peptide nanotubes, formed by a lugdunin self-assembly in lipid membranes, comprise a water-filled membrane pore capable of transporting protons. For further support, single-channel proton conductance measurements would be ...
formed by a lugdunin self-assembly in lipid membranes, comprise a water-filled membrane pore capable of transporting protons. For further support, single-channel proton conductance measurements would be desirable but cannot be performed at physiological conditions owing to orders of magnitudes ...
Emergence of Crops in Clay Soils of the Central Sudan Rainlands in Relation to Soil Water and Air-Filled Pore Space Poor emergence of crops is common during the rainy season on the clay soils of the central Sudan.Arachis hypogaea, Sesamum indicum, Hibiscus cannabinusandG... HRB Hack - 《Ex...
The percentage of soil pore space filled with water (percent water-filled pores, % WFP), as determined by water content and total porosity, appears to be closely related to soil microbial activity under different tillage regimes. Soil incubated in the laboratory at 60% WFP supported maximum ...
Dobbie, KE, Smith, KA (2001) The effects of temperature, water-filled pore space and land use on N2O emissions from an imperfectly drained gleysol. Eur J Soil Sci 52: pp. 667-673Dobbie KE, Smith KA (2001) The effects of temperature, water-filled pore space and land use on N 2 O ...
Soil dissolved organic carbon: Influences of water-filled pore space and red clover addition and relationships with microbial biomass carbon. Can. J. Soil Sci. 84:151-158. doi:10.4141/S02-030Zhang TQ, Drury CF, Kay BD 2004: Soil dissolved organic carbon: Influences of water-filled pore ...
Mekala C, Nambi I M. 2017. Understanding the hydrologic control of N cycle: Effect of water filled pore space on heterotrophic nitrification, denitrification and dissimilatory nitrate reduction to ammonium mechanisms in unsaturated soils [ J] . Journal of Contaminant Hydrology, 202: 11⁃22...
Emission of N 2 O and CH 4 oxidation rates were measured from soils of contrasting (30–75%) water-filled pore space (WFPS). Oxidation rates of 13 C–CH 4 were determined after application of 10 μl 13 C–CH 4 l 1 (10 at. % excess 13 C) to soil headspace and comparisons made...