Carbon, Nitrogen and Phosphorus Cycling in Forest Soils

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...

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Bibliographic Details
Main Author: Qualls, Robert G. (auth)
Format: Electronic Book Chapter
Language:English
Published: MDPI - Multidisciplinary Digital Publishing Institute 2019
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520 |a 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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650 7 |a Biology, life sciences  |2 bicssc 
653 |a polyphenols 
653 |a aluminum accumulator 
653 |a near natural forest management 
653 |a chloroform fumigation extraction 
653 |a soil structure 
653 |a soil enzymes 
653 |a manure pelleting 
653 |a microbial biomass 
653 |a Oxisol 
653 |a biolability 
653 |a soil nutrients 
653 |a second production cycle 
653 |a PLFA 
653 |a pyrolysis 
653 |a Eucalyptus sp. 
653 |a Cunninghamia lanceolata plantation 
653 |a carbon 
653 |a the Three Gorges Reservoir 
653 |a revegetation 
653 |a carbon distribution index 
653 |a climate change 
653 |a seasons 
653 |a annual increment average 
653 |a topography 
653 |a humic substances 
653 |a litter N 
653 |a soil fertility 
653 |a climate zone 
653 |a nutrient cycling 
653 |a Daxing'an Mountains 
653 |a carbon mineralization 
653 |a nitrification 
653 |a 31P nuclear magnetic resonance spectroscopy (31P NMR) 
653 |a organic matter 
653 |a throughfall 
653 |a forest soil 
653 |a dissolved organic carbon (DOC) 
653 |a P species 
653 |a stoichiometric homeostasis 
653 |a dissolved organic matter (DOM) 
653 |a soil organic matter fraction 
653 |a variable-charge soils 
653 |a ammonium 
653 |a nitrate 
653 |a soil degradation 
653 |a soil P fractions 
653 |a seasonal trends 
653 |a ammonia-oxidizing bacteria 
653 |a nitrogen dynamics 
653 |a net primary productivity 
653 |a soil microbial communities 
653 |a beech forests 
653 |a soil pH 
653 |a wood volume 
653 |a temperature 
653 |a northern temperate 
653 |a multilevel models 
653 |a Pinus massoniana plantation 
653 |a ammonia-oxidizing archaea 
653 |a P stock 
653 |a stand density 
653 |a P resorption efficiency 
653 |a forest types 
653 |a soil greenhouse gas flux 
653 |a enzyme activities 
653 |a soil N 
653 |a alpine forest 
653 |a moisture gradient 
653 |a climate 
653 |a climatic factors 
653 |a soil available phosphorus 
653 |a microbial activity 
653 |a soil available nitrogen 
653 |a leaf N:P ratio 
653 |a stemflow 
653 |a Chamaecyparis forest 
653 |a charcoal 
653 |a gross nitrogen transformations 
653 |a principal component analyses 
653 |a information review 
653 |a manuring 
653 |a stand age 
653 |a tree-DOM 
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