The use of ignition loss to estimate bulk density of forest soils

1989 ◽  
Vol 40 (2) ◽  
pp. 299-308 ◽  
Author(s):  
J. L. HONEYSETT ◽  
D. A. RATKOWSKY
2011 ◽  
Vol 28 (4) ◽  
pp. 194-198 ◽  
Author(s):  
Oscar Bustos ◽  
Andrew Egan

Abstract A study of soil compaction associated with four harvesting systems—a forwarder working with a mechanized harvester and a rubber-tired cable skidder, a farm tractor, and a bulldozer, each of them coupled with a chainsaw felling—was conducted in a group selection harvest of a mixed hardwood stand in Maine. The bulldozer system was associated with the highest percentage differences in soil bulk density measured in machine tracks (16.9%), trail centerlines (15.7%), and harvested group selection units (13.1%) versus adjacent untrafficked areas, whereas the forwarder system was associated with the lowest percentage differences in soil bulk density measured in machine tracks (3.5%), trail centerlines (1.2%), and harvested group selection units (6.3%) versus adjacent untrafficked areas. Results will help to inform loggers and foresters on equipment selection, harvest planning, and the conservation of forest soils and soil productivity.


Author(s):  
Oksana Lenevych ◽  
Zinoviy Pankiv

Carry out monitoring of the track “Skole−Parashka” by the main five criteria of degradation of the natural environment: 1) width track (І category: to 0,5 m, “Unchanged track”; II category: to 1 m, “Little−changed track”; III category: 2−3 m “Endangered track”; IV category: to 5 m “Devastated track”; V category: over 5 m, “Strongly devastated track”); 2) presence of additional/parallel paths; 3) soil density; 4) quantitative and qualitative changes in vegetation (meadow ecosystems), presence/absence of forest litter (forest ecosystems); 5) the growth of erosion processes and the microrelief of the trail. It was found that for 10 years of exploitation by tourist track “Skole − Parashka” the width of the trail increased by 0,3–1,2 m. Reveal changes in soil over physical, water-physical, physicо-chemical and biotic properties of brown forest soils. The bulk density of soil structure on trails during 2012−2014 increased by approximately 32 % compared to the control, and after 10 years it increased − to 38 %. To reveal within the roadside an increase in soil bulk density from 1,07 to 1,17 g•cm-³ for 2019−2021 years. An increase in the density of the solid phase was recorded. The results of which are characteristic of the Hp horizon of brown forest soils. On the track porosity total to appraise “unsatisfactory”. For 10 years of recreational use of the track, the water permeability on the trails has not changed and was 0,07 and 0,06 mm•min-¹ according to the periods of the study (2012-2014 and 2019-2021). Within the roadside water permeability in 2012−2014 decreased by 60−80%, then in 2019−2021 years water permeability decreased by more than 90%. The actual water permeability of the soil during the downpour rains causes the intensification of surface runoff on the trail. On the track reveal abatement C organic. On the roadside track when lay to plane surface C organic unchanged within a years (2012−2014 and 2019−2021) and even was outstanding within a control. The increase C organic on the roadside is a result of “penetration” of the crushed fractions of forest litter into the H horizon during trampling and is not the result of biochemical processes. On the track increase of soil reaction (pH 5,0) while in the control pH 4,0. As to the biotic activity parameters, among the most significant are the catalase activity indices which are mostly determined by the density of the soil structure and water permeability. Key words: soil bulk density; water permeability; C organic; biotic activity; recreation influence; monitoring; NPP “Skolivski Beskydy”.


Author(s):  
Oksana Lenevych

The article analyses the influence of recreational load on the physical and water-physical properties of brown forest soils. It is established that the complete or partial absence of litter on the pathway contributes to the rapid evaporation of moisture from the upper horizon (0−5 cm) of the soil, reducing the porosity total, increasing the density solid phase and buk density. It was found that with the increase of the buk density by 12,5 % the water permeability of the soil decreases 33 times in comparison with the control. A significant increase in the bulk density of the structure by 39−48 % was found on partway with a width of more than 2 m. On these pathway the surface runoff of water is formed. An increase in the density of the solid phase was recorded. The results of which are characteristic of the Hp horizon of brown forest soils. The overlapping of the trail with wooden flooring on the track “Stezhkamy lehendarnoyi Tustani” had a positive effect on the physical and water-physical properties of the soil. It was found that the indicators of soil bulk density and water permeability were close to the results obtained in the control and only the increase in the density of the solid phase indicates a significant recreational impact in the past. On the roadsides of the same revealed a significant increase in soil density of 1,5 times compared to the control and 1,3 times with the results obtained on the pathway, this indicates a recreational impact to date. It is proposed to use the following criteria for degradation of natural ecosystem: quantitative and qualitative changes in vegetation (meadow ecosystems), presence/absence of forest litter (forest ecosystems), soil density, presence of additional/parallel paths, path width, depth of erosion on the pathway. Establish category (stages) of recreational degression on the tracks the National Park “Skolivski Beskydy”. On the first stage/category (“Unchanged track”) of recreational degression includes trails 0,35−0,70 m wide with relatively close indicators of soil structure bulk density to control and the presence of forest litter on the pathway. The only negative aspect in this category is the insufficient water permeability of the soil. On heavy II category there is forest litter, although its redistribution is mainly traced between the trail and its roadside. In some sections of the trail, where there is no forest litter, it is fixed by increasing the bulk density of the structure to 27 %, the width of the pathway is 0,9−1,2 m and is classified as “Little-changed track”. On pathway with 2,15−3,40 m, there is a complete or partial absence of forest litter. Bulk density increased by 38−39 %, surface water runoff is formed. It is established presence distinct partway, visibled qualitative and quantitative changes in vegetation. The presented data correspond to the pathway of III category and are classified as “Endangered track”. Category IV (“Devastated track”) includes paths on which there is no forest litter, a significant increase in soil density up to 48 %, access to the surface of the root system and the width of the path is 2,60−4,90 m. Key words: recreation influence; soil bulk density; water permeable; pathway; NPP “Skolivski Beskydy”.


2016 ◽  
Vol 80 (3) ◽  
pp. 756-764 ◽  
Author(s):  
Youzhi Han ◽  
Jianwei Zhang ◽  
Kim G. Mattson ◽  
Weidong Zhang ◽  
Thomas A. Weber

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