Thaw depth determines reaction and transport of inorganic nitrogen in valley bottom permafrost soils: Nitrogen cycling in permafrost soils.
about
The unseen iceberg: plant roots in arctic tundra.Pronounced chemical response of Subarctic lakes to climate-driven losses in surface area.Permafrost collapse alters soil carbon stocks, respiration, CH4 , and N2O in upland tundra.Convergence of soil nitrogen isotopes across global climate gradients.NifH-Harboring Bacterial Community Composition across an Alaskan Permafrost Thaw Gradient.Experimentally increased nutrient availability at the permafrost thaw front selectively enhances biomass production of deep-rooting subarctic peatland species.Nitrate is an important nitrogen source for Arctic tundra plants.Hydraulic redistribution by plants and nutrient stoichiometry: Shifts under global changeEcological interpretations of nitrogen isotope ratios of terrestrial plants and soilsEstimated storage of amorphous silica in soils of the circum-Arctic tundra region
P2860
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P2860
Thaw depth determines reaction and transport of inorganic nitrogen in valley bottom permafrost soils: Nitrogen cycling in permafrost soils.
description
2012 nî lūn-bûn
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2012年の論文
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2012年論文
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2012年論文
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2012年論文
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2012年論文
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2012年論文
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2012年论文
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2012年论文
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name
Thaw depth determines reaction ...... n cycling in permafrost soils.
@en
Thaw depth determines reaction ...... n cycling in permafrost soils.
@nl
type
label
Thaw depth determines reaction ...... n cycling in permafrost soils.
@en
Thaw depth determines reaction ...... n cycling in permafrost soils.
@nl
prefLabel
Thaw depth determines reaction ...... n cycling in permafrost soils.
@en
Thaw depth determines reaction ...... n cycling in permafrost soils.
@nl
P2860
P1476
Thaw depth determines reaction ...... n cycling in permafrost soils.
@en
P2093
Jeremy B Jones
Tamara K Harms
P2860
P304
P356
10.1111/J.1365-2486.2012.02731.X
P577
2012-06-12T00:00:00Z