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in forest
Nitrate has been recognized as the dominant mineral nitrogen form in most agricultural soils and the main nitrogen source for crops, but it is not usually the case in forest ecosystems.
      
Fine root lifespan and turnover play an important role in carbon allocation and nutrient cycling in forest ecosystems.
      
Soil properties in forest gaps and under canopy in broad-leaved Pinus koraiensis forests in Changbai Mountainous Region, China
      
Results showed that compared with farmland watersheds, runoff generation time in forest watersheds was delayed remarkably, and peak flow was reduced greatly, which indicates that vegetation played an important role in holding and absorbing rainfall.
      
The two forests differ in forest humus layer; it is deep in the Ailao forest while little is present in the Xishuangbanna forest.
      
Fine root turnover plays important roles in carbon allocation and nutrient cycling in forest ecosystems.
      
Forest precipitation chemistry is a major issue in forest hydrology and forest ecology.
      
However, the sustainability capacity was still lower than those in forest developed countries.
      
Effects of elevated CO2 concentrations on soil microbial respiration and root/rhizosphere respiration in forest soils
      
Concept and Classification of Coarse Woody Debris in Forest Ecosystems
      
However, the definition and classification of CWD have been the subject of a long debate in forest ecology.
      
Soil animals are abundant in forest litter layer, but little attention has been paid to the vertical distribution of community structure of soil animals in the layers at different plant community succession stages.
      
Maximum wind velocity (Vmax) and photo effective radiation in forest edges were higher than those in interior forest, which presented a stronger temperature-gained edge effect.
      
The Recent Trend of the Biodiversity Dynamic of Biotic Communities in Forest-Steppe Oak Forests
      
The effect of forest fires differing in intensity on organic matter dynamics in forest soils has been assessed in different types of forest sites using the EFIMOD system of models.
      
In forest phytocenosis that were formed with species replacement (after cuttings with understory clearing), the annual moss production (net primary production) ranged from 2.8 to 20.6 g/(m2 y).
      
Effect of emissions from a Copper-Nickel Smelter on soil microbial communities in forest biogeocenoses of the Kola Peninsula
      
Community Structure of Yeast Fungi in Forest Biogeocenoses
      
The yeast diversity in forest biogeocenoses is shown to surpass that in other geographic zones.
      
The taxonomic structure of yeast communities was studied in forest litter and soil, as well as in substrates transformed by the activity of Lumbricus terrestris earthworms (leaves in heaps, the gut contents, and coproliths).
      
 

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