Preliminary assessment of the impact of (2)
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We compared organic carbon and total nitrogen pools in forest floor and mineral soil (0–100-cm depth) in three areas burned by local communities (B) with adjacent unburned areas
The soil pH, organic carbon, exchangeable Na, K, Ca and Mg, total and available P, K, S contents of soil increased significantly with increasing levels ef phosphorus and sulphur
Though there was a gradual decline of both organic carbon and available N at 35 days after incorporation, decomposed banana peduncle, decomposed waste tender coconut, mushroom spent
Soil N2O Emission in Relation to Soil Property Increasing soil temperature, organic carbon, pH, available nitrogen, and total nitrogen was significantly promoted, but increasing soil
44 3.7 Main effects of earthworms, litter and temperature on soil organic carbon and soil total nitrogen at the end of incubation 4.1 Organic carbon, total nitrogen and pH of soil
3 Relationships between the concentrations of total soil sulfur andatotal soil carbon,btotal soil nitrogen, andcsoil organic phosphorus P, in mineral and organic horizons of soils along
Similarly, soil organic matter, total nitrogen, available phosphorus, and cation exchange capacity were significantly P < 0.05 influenced by the combined effects of land management
3 Seasonal changes in the ratios of microbial carbon to nitrogen a, carbon to phosphorus b, and nitrogen to phosphorus c following a decade of fertilization of a lowland tropical forest
