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Carbon, Nitrogen and Phosphorus Cycling in Forest Soils
Robert G. Qualls
2019
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The majority of carbon stored in the soils of the world is stored in forests. The refractory nature of some portions of forest soil organic matter also provides the slow, gradual release of organic nitrogen and phosphorus to sustain long term forest productivity. Contemporary and future disturbances, such as climatic warming, deforestation, short rotation sylviculture, the invasion of exotic species, and fire, all place strains on the integrity of this homeostatic system of C, N, and P cycling. On the other hand, the CO2 fertilization effect may partially offset losses of soil organic matter, but many have questioned the ability of N and P stocks to sustain the CO2 fertilization effect.
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Keywords
- 31P nuclear magnetic resonance spectroscopy (31P NMR)
- alpine forest
- aluminum accumulator
- ammonia-oxidizing archaea
- ammonia-oxidizing bacteria
- ammonium
- annual increment average
- beech forests
- biolability
- Carbon
- carbon distribution index
- carbon mineralization
- Chamaecyparis forest
- charcoal
- chloroform fumigation extraction
- Climate
- Climate Change
- climate zone
- Climatic Factors
- Cunninghamia lanceolata plantation
- Daxing’an Mountains
- dissolved organic carbon (DOC)
- dissolved organic matter (DOM)
- enzyme activities
- Eucalyptus sp.
- forest soil
- forest types
- gross nitrogen transformations
- humic substances
- information review
- leaf N:P ratio
- litter N
- manure pelleting
- manuring
- microbial activity
- microbial biomass
- moisture gradient
- multilevel models
- near natural forest management
- net primary productivity
- nitrate
- Nitrification
- nitrogen dynamics
- northern temperate
- Nutrient Cycling
- organic matter
- Oxisol
- P resorption efficiency
- P species
- P stock
- Pinus massoniana plantation
- PLFA
- Polyphenols
- principal component analyses
- pyrolysis
- revegetation
- seasonal trends
- Seasons
- second production cycle
- soil available nitrogen
- soil available phosphorus
- soil degradation
- soil enzymes
- Soil fertility
- soil greenhouse gas flux
- soil microbial communities
- soil N
- soil nutrients
- soil organic matter fraction
- soil P fractions
- soil pH
- soil structure
- stand age
- stand density
- stemflow
- stoichiometric homeostasis
- temperature
- the Three Gorges Reservoir
- throughfall
- topography
- tree-DOM
- variable-charge soils
- wood volume
Links
DOI: 10.3390/books978-3-03897-683-7Editions
