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...
Kaydedildi:
| Yazar: | |
|---|---|
| Materyal Türü: | Online |
| Dil: | İngilizce |
| Baskı/Yayın Bilgisi: |
MDPI - Multidisciplinary Digital Publishing Institute
2021
|
| Konular: | |
| Online Erişim: | 33698 |
| Etiketler: |
Etiket eklenmemiş, İlk siz ekleyin!
|
| _version_ | 1869522422832562176 |
|---|---|
| author | Qualls, Robert G. |
| author_browse | Qualls, Robert G. |
| author_facet | Qualls, Robert G. |
| author_sort | Qualls, Robert G. |
| collection | Directory of Open Access Books |
| description | 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. |
| format | Online |
| id | doab-20.500.12854ir-42702 |
| institution | Directory of Open Access Books |
| language | eng |
| publishDate | 2021 |
| publishDateRange | 2021 |
| publishDateSort | 2021 |
| publisher | MDPI - Multidisciplinary Digital Publishing Institute |
| publisherStr | MDPI - Multidisciplinary Digital Publishing Institute |
| record_format | ojs |
| spelling | doab-20.500.12854ir-427022024-04-05T12:32:45Z Carbon, Nitrogen and Phosphorus Cycling in Forest Soils Qualls, Robert G. QH301-705.5 Q1-390 SD1-669.5 polyphenols aluminum accumulator near natural forest management chloroform fumigation extraction soil structure soil enzymes manure pelleting microbial biomass Oxisol biolability soil nutrients second production cycle PLFA pyrolysis Eucalyptus sp. Cunninghamia lanceolata plantation carbon the Three Gorges Reservoir revegetation carbon distribution index climate change seasons annual increment average topography humic substances litter N soil fertility climate zone nutrient cycling Daxing’an Mountains carbon mineralization nitrification 31P nuclear magnetic resonance spectroscopy (31P NMR) organic matter throughfall forest soil dissolved organic carbon (DOC) P species stoichiometric homeostasis dissolved organic matter (DOM) soil organic matter fraction variable-charge soils ammonium nitrate soil degradation soil P fractions seasonal trends ammonia-oxidizing bacteria nitrogen dynamics net primary productivity soil microbial communities beech forests soil pH wood volume temperature northern temperate multilevel models Pinus massoniana plantation ammonia-oxidizing archaea P stock stand density P resorption efficiency forest types soil greenhouse gas flux enzyme activities soil N alpine forest moisture gradient climate climatic factors soil available phosphorus microbial activity soil available nitrogen leaf N:P ratio stemflow Chamaecyparis forest charcoal gross nitrogen transformations principal component analyses information review manuring stand age tree-DOM thema EDItEUR::P Mathematics and Science::PS Biology, life sciences 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. 2021-02-11T09:30:57Z 2021-02-11T09:30:57Z 2019-06-26 08:44:06 2019 book 33698 9783038976837 9783038976820 https://directory.doabooks.org/handle/20.500.12854/42702 eng image/jpeg Attribution-NonCommercial-NoDerivatives 4.0 International https://mdpi.com/books/pdfview/book/1367 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-03897-683-7 10.3390/books978-3-03897-683-7 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783038976837 9783038976820 238 open access |
| spellingShingle | QH301-705.5 Q1-390 SD1-669.5 polyphenols aluminum accumulator near natural forest management chloroform fumigation extraction soil structure soil enzymes manure pelleting microbial biomass Oxisol biolability soil nutrients second production cycle PLFA pyrolysis Eucalyptus sp. Cunninghamia lanceolata plantation carbon the Three Gorges Reservoir revegetation carbon distribution index climate change seasons annual increment average topography humic substances litter N soil fertility climate zone nutrient cycling Daxing’an Mountains carbon mineralization nitrification 31P nuclear magnetic resonance spectroscopy (31P NMR) organic matter throughfall forest soil dissolved organic carbon (DOC) P species stoichiometric homeostasis dissolved organic matter (DOM) soil organic matter fraction variable-charge soils ammonium nitrate soil degradation soil P fractions seasonal trends ammonia-oxidizing bacteria nitrogen dynamics net primary productivity soil microbial communities beech forests soil pH wood volume temperature northern temperate multilevel models Pinus massoniana plantation ammonia-oxidizing archaea P stock stand density P resorption efficiency forest types soil greenhouse gas flux enzyme activities soil N alpine forest moisture gradient climate climatic factors soil available phosphorus microbial activity soil available nitrogen leaf N:P ratio stemflow Chamaecyparis forest charcoal gross nitrogen transformations principal component analyses information review manuring stand age tree-DOM thema EDItEUR::P Mathematics and Science::PS Biology, life sciences Qualls, Robert G. Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title | Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title_full | Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title_fullStr | Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title_full_unstemmed | Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title_short | Carbon, Nitrogen and Phosphorus Cycling in Forest Soils |
| title_sort | carbon nitrogen and phosphorus cycling in forest soils |
| topic | QH301-705.5 Q1-390 SD1-669.5 polyphenols aluminum accumulator near natural forest management chloroform fumigation extraction soil structure soil enzymes manure pelleting microbial biomass Oxisol biolability soil nutrients second production cycle PLFA pyrolysis Eucalyptus sp. Cunninghamia lanceolata plantation carbon the Three Gorges Reservoir revegetation carbon distribution index climate change seasons annual increment average topography humic substances litter N soil fertility climate zone nutrient cycling Daxing’an Mountains carbon mineralization nitrification 31P nuclear magnetic resonance spectroscopy (31P NMR) organic matter throughfall forest soil dissolved organic carbon (DOC) P species stoichiometric homeostasis dissolved organic matter (DOM) soil organic matter fraction variable-charge soils ammonium nitrate soil degradation soil P fractions seasonal trends ammonia-oxidizing bacteria nitrogen dynamics net primary productivity soil microbial communities beech forests soil pH wood volume temperature northern temperate multilevel models Pinus massoniana plantation ammonia-oxidizing archaea P stock stand density P resorption efficiency forest types soil greenhouse gas flux enzyme activities soil N alpine forest moisture gradient climate climatic factors soil available phosphorus microbial activity soil available nitrogen leaf N:P ratio stemflow Chamaecyparis forest charcoal gross nitrogen transformations principal component analyses information review manuring stand age tree-DOM thema EDItEUR::P Mathematics and Science::PS Biology, life sciences |
| topic_facet | QH301-705.5 Q1-390 SD1-669.5 polyphenols aluminum accumulator near natural forest management chloroform fumigation extraction soil structure soil enzymes manure pelleting microbial biomass Oxisol biolability soil nutrients second production cycle PLFA pyrolysis Eucalyptus sp. Cunninghamia lanceolata plantation carbon the Three Gorges Reservoir revegetation carbon distribution index climate change seasons annual increment average topography humic substances litter N soil fertility climate zone nutrient cycling Daxing’an Mountains carbon mineralization nitrification 31P nuclear magnetic resonance spectroscopy (31P NMR) organic matter throughfall forest soil dissolved organic carbon (DOC) P species stoichiometric homeostasis dissolved organic matter (DOM) soil organic matter fraction variable-charge soils ammonium nitrate soil degradation soil P fractions seasonal trends ammonia-oxidizing bacteria nitrogen dynamics net primary productivity soil microbial communities beech forests soil pH wood volume temperature northern temperate multilevel models Pinus massoniana plantation ammonia-oxidizing archaea P stock stand density P resorption efficiency forest types soil greenhouse gas flux enzyme activities soil N alpine forest moisture gradient climate climatic factors soil available phosphorus microbial activity soil available nitrogen leaf N:P ratio stemflow Chamaecyparis forest charcoal gross nitrogen transformations principal component analyses information review manuring stand age tree-DOM thema EDItEUR::P Mathematics and Science::PS Biology, life sciences |
| url | 33698 |
| work_keys_str_mv | AT quallsrobertg carbonnitrogenandphosphoruscyclinginforestsoils |