Invertebrate herbivory in the forest floor vegetation of virgin and managed forest sites in the Kibale Forest, western Uganda

1992 ◽  
Vol 30 (3) ◽  
pp. 213-222 ◽  
Author(s):  
MATTI NUMMELIN
Keyword(s):  
Forest Floor ◽  
Managed Forest ◽  
Kibale Forest ◽  
Forest Sites ◽  
Western Uganda ◽  
Forest Floor Vegetation ◽  
Invertebrate Herbivory

Long-term forest utilization can decrease forest floor microhabitat diversity: evidence from boreal Fennoscandia

2004 ◽  
Vol 34 (2) ◽  
pp. 303-309 ◽  
Author(s):  
Timo Kuuluvainen ◽  
Raija Laiho
Keyword(s):  
Forest Floor ◽  
Natural Forest ◽  
Decayed Wood ◽  
Natural Forests ◽  
Managed Forest ◽  
Vegetation Zone ◽  
Forest Sites ◽  
History Of ◽  
Forest Utilization

Forest floor microhabitat diversity was studied in old Pinus sylvestris L. dominated forest sites in two regions within the middle boreal vegetation zone in Fennoscandia: in 50 managed forest sites in the Häme region in southwestern Finland and in 45 natural or old selectively logged forest sites in the Kuhmo–Viena region in northeastern Finland and northwestern Russia. The forests in the Häme region are characterized by a long history of forest utilization, while the forests in the Kuhmo–Viena region can be regarded as natural or near natural. The managed forest sites in Häme had significantly lower forest floor microhabitat diversity compared with natural and near-natural forests. Microhabitats that were significantly more scarce in managed versus natural and near-natural forest sites included humps, depressions, decayed wood, and vicinity of decayed wood. On the other hand, even ground was significantly more abundant in managed forest compared with natural and near-natural forest. Microhabitat availability was also reflected in the occurrence of tree saplings growing in different microhabitats. The results suggest that long-term forest utilization has decreased forest floor microhabitat diversity. This has occurred because of a decreased amount of fallen deadwood and, possibly, lack of soil disturbances because of fewer uprootings caused by falling trees.

scholarly journals Atmospheric Heavy Metal Input to Forest Soils in Rural Areas of Denmark

2007 ◽  
Vol 7 ◽  
pp. 192-197 ◽  
Author(s):  
M. F. Hovmand ◽  
Kaare Kemp
Keyword(s):  
Heavy Metals ◽  
Heavy Metal ◽  
Rural Areas ◽  
Forest Floor ◽  
Ambient Atmosphere ◽  
Chronological Order ◽  
Forest Sites ◽  
Yearly Average ◽  
Atmospheric Inputs

Atmospheric bulk deposition of heavy metals (HM) was measured from 1972/73 to the present time at five to ten forest sites in rural areas of Denmark. From 1979, HM in aerosols were measured at one to four forest sites. On the basis of these long-term continuous measurements, the atmospheric inputs to the forest floor have been calculated. Yearly HM emission estimates to the European atmosphere seems to correlate well with yearly average values of HM deposition, as well as with HM concentrations in the ambient atmosphere. HM emissions have been estimated since the 1950s. Using the correlation between emission and deposition, HM deposition values maybe extrapolated in reverse chronological order. The accumulated atmospheric HM deposition has been estimated in this way over a period of 50 years.

scholarly journals Decoupling of a Douglas fir canopy: a look into the subcanopy with continuous vertical temperature profiles

2020 ◽  
Vol 17 (24) ◽  
pp. 6423-6439
Author(s):  
Bart Schilperoort ◽  
Miriam Coenders-Gerrits ◽  
César Jiménez Rodríguez ◽  
Christiaan van der Tol ◽  
Bas van de Wiel ◽  
...  
Keyword(s):  
Forest Floor ◽  
Thermal Stratification ◽  
Douglas Fir ◽  
Temperature Profiles ◽  
Distributed Temperature Sensing ◽  
Vertical Temperature ◽  
Vertical Exchange ◽  
Forest Sites ◽  
Flux Measurements ◽  
Atmosphere Interaction

Abstract. Complex ecosystems such as forests make accurately measuring atmospheric energy and matter fluxes difficult. One of the issues that can arise is that parts of the canopy and overlying atmosphere can be turbulently decoupled from each other, meaning that the vertical exchange of energy and matter is reduced or hampered. This complicates flux measurements performed above the canopy. Wind above the canopy will induce vertical exchange. However, stable thermal stratification, when lower parts of the canopy are colder, will hamper vertical exchange. To study the effect of thermal stratification on decoupling, we analyze high-resolution (0.3 m) vertical temperature profiles measured in a Douglas fir stand in the Netherlands using distributed temperature sensing (DTS). The forest has an open understory (0–20 m) and a dense overstory (20–34 m). The understory was often colder than the atmosphere above (80 % of the time during the night, >99 % during the day). Based on the aerodynamic Richardson number the canopy was regularly decoupled from the atmosphere (50 % of the time at night). In particular, decoupling could occur when both u*<0.4 m s−1 and the canopy was able to cool down through radiative cooling. With these conditions the understory could become strongly stably stratified at night. At higher values of the friction velocity the canopy was always well mixed. While the understory was nearly always stably stratified, convection just above the forest floor was common. However, this convection was limited in its vertical extent, not rising higher than 5 m at night and 15 m during the day. This points towards the understory layer acting as a kind of mechanical “blocking layer” between the forest floor and overstory. With the DTS temperature profiles we were able to study decoupling and stratification of the canopy in more detail and study processes which otherwise might be missed. These types of measurements can aid in describing the canopy–atmosphere interaction at forest sites and help detect and understand the general drivers of decoupling in forests.

Nitrogen-retention capacity in a fertilized forest after clear-cutting — the effect of forest-floor vegetation

2015 ◽  
Vol 45 (1) ◽  
pp. 130-134 ◽  
Author(s):  
Per-Ola Hedwall ◽  
Johan Bergh ◽  
Annika Nordin
Keyword(s):  
Vegetation Cover ◽  
Forest Floor ◽  
Nitrogen Retention ◽  
Tree Seedling ◽  
Retention Capacity ◽  
N Retention ◽  
Clear Cutting ◽  
Nitrate N ◽  
Ammonium N ◽  
Forest Floor Vegetation

Forest fertilization with nitrogen (N) has several benefits to society such as increased wood production and carbon sequestration. There are, however, concerns about N leakage, particularly following clear-cutting. The forest-floor vegetation may increase the N retention of forest ecosystems; however, very few studies have quantified the amount of vegetation required. We studied the relationship between vegetation cover and risk of N leakage, estimated by the amounts of ammonium-N and nitrate-N retained on ion-exchange capsules in the soil, during 4 years following the clear-cutting and harvesting of logging residues in a previously fertilized forest in southern Sweden. Previous fertilization increased the amount of nitrate-N captured on the capsules, whereas the amount of ammonium-N decreased. The vascular vegetation cover increased from almost zero to approximately 25% independent of fertilization. The amount of ammonium-N and nitrate-N retained on the capsules was already reduced by 50%–75% at 20% vegetation cover, and by 30%–40% cover, it approached zero, independent of the number of years since clear-cutting. The vegetation may impede tree-seedling establishment, implying a trade-off between seedling growth and N-retention capacity. However, our results indicate that maximum N retention may be achieved at a relatively low vegetation cover, which could be accomplished with less intrusive scarification methods than currently used.

Metapopulation dynamics of a beetle species confined to burned forest sites in a managed forest region

Ecography ◽  
2014 ◽  
Vol 37 (8) ◽  
pp. 797-804 ◽  
Author(s):  
Thomas Ranius ◽  
Petter Bohman ◽  
Olof Hedgren ◽  
Lars-Ove Wikars ◽  
Alexandro Caruso
Keyword(s):  
Metapopulation Dynamics ◽  
Beetle Species ◽  
Managed Forest ◽  
Forest Region ◽  
Forest Sites ◽  
Burned Forest

scholarly journals Multiple environmental changes drive forest floor vegetation in a temperate mountain forest

2017 ◽  
Vol 7 (7) ◽  
pp. 2155-2168 ◽  
Author(s):  
Norbert Helm ◽  
Franz Essl ◽  
Michael Mirtl ◽  
Thomas Dirnböck
Keyword(s):  
Forest Floor ◽  
Environmental Changes ◽  
Mountain Forest ◽  
Forest Floor Vegetation

Termites (Isoptera) in Kibale Forest National Park, Western Uganda

1997 ◽  
Vol 86 (1) ◽  
pp. 51-59
Author(s):  
J. P. E. C. Darlington ◽  
M. Leponce ◽  
W. O. Ogutu
Keyword(s):  
National Park ◽  
Kibale Forest ◽  
Western Uganda
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