A5051469173- Soil Carbon and Nitrogen Dynamics
- Soil and Water Nutrient Dynamics
- Plant nutrient uptake and metabolism
- Legume Nitrogen Fixing Symbiosis
- Isotope Analysis in Ecology
- Groundwater and Isotope Geochemistry
- Agronomic Practices and Intercropping Systems
- Phosphorus and nutrient management
- Wastewater Treatment and Nitrogen Removal
- Agriculture, Soil, Plant Science
- Soybean genetics and cultivation
- Ruminant Nutrition and Digestive Physiology
- Crop Yield and Soil Fertility
- Geology and Paleoclimatology Research
- Growth and nutrition in plants
- Plant Micronutrient Interactions and Effects
- Aluminum toxicity and tolerance in plants and animals
- Rice Cultivation and Yield Improvement
- Analytical Chemistry and Chromatography
- Peatlands and Wetlands Ecology
- Radioactive contamination and transfer
- Plant Taxonomy and Phylogenetics
- Genetic and Environmental Crop Studies
- Clay minerals and soil interactions
- Mass Spectrometry Techniques and Applications
The University of Melbourne
2008-2022
Commonwealth Scientific and Industrial Research Organisation
1994-2020
Research Center for Eco-Environmental Sciences
2016-2020
Chinese Academy of Sciences
2016-2020
Brazilian Agricultural Research Corporation
1983-2017
Instituto de Pesquisas Jardim Botânico do Rio de Janeiro
2013-2017
International Atomic Energy Agency
2000-2012
International Rice Research Institute
1999-2002
Plant Industry
1995
Universidade de São Paulo
1990
After decades of searching for a rapid method to estimate the N mineralization capacity soil, there is still no consistent recommendation. It legitimate examine causes often‐conflicting results in literature. The efficacy various references that have been used as benchmarks assessing chemical and physical indices literature critically reviewed this paper. Gross consumption during waterlogged aerobic incubations were estimated wide range soils. was found equivalent 17 90 23 59% mineralized...
Abstract The biological oxidation of NO 2 ‐ is inhibited when alkaline‐hydrolyzing N fertilizers are band‐applied to soils, and may accumulate. Nitrogenous gases can be evolved with added soil. aim the work described here was determine if gaseous‐N losses could occur via chemical transformations during nitrification in soils treated NH 3 fertilizer. Evolution , O, + occurred three aqueous . Losses measured soil pH > 7.5. highest loss amounted 16.5% applied‐N (1156 µg applied/g soil) a...
Abstract When alkaline‐hydrolyzing N fertilizers are band‐applied to soils, the biological oxidation of NO 2 ‐ is inhibited and may accumulate. Nitrite can react chemically with soil organic matter become fixed, at same time nitrogenous gases be evolved. The aim work described here was study mechanisms gaseous‐N formation using 15 as a tracer, define relationship between fixation loss N. Fixation Na in five soils varying pH C content ranged from 0.6 36% applied , while not recovered varied 6...