scholarly journals Reducing Sediments from Skid Roads in West Virginia Using Fiber Mats

2009 ◽  
Vol 26 (3) ◽  
pp. 118-121 ◽  
Author(s):  
Shawn T. Grushecky ◽  
Ben D. Spong ◽  
David W. McGill ◽  
John W. Edwards

Abstract A research study was established to test the effectiveness of fiber mats and native seed mixtures in reducing soil erosion from newly constructed skid roads in the Elk River watershed in central West Virginia. Six road sections received fiber mat and native grass seed and were pairedwith randomly selected sections of equal grade receiving no treatments. Silt fences with sediment traps were constructed at the downslope terminus of each road section. Sediments were collected from silt traps three times during summer 2005 and 2006. Over the 2-year study period, sedimentswere reduced by 88% on skid trails treated with fiber mats and seeding. Our findings suggest that the use of fiber mats has the potential to significantly reduce sedimentation from skid roads in West Virginia.

2020 ◽  
Vol 38 (4) ◽  
pp. 237-245
Author(s):  
Forrest S. Smith ◽  
Jon Paul Pierre ◽  
Michael H. Young ◽  
Dale A. Devitt

2010 ◽  
Vol 14 (4) ◽  
pp. 675-686 ◽  
Author(s):  
N. Konz ◽  
D. Baenninger ◽  
M. Konz ◽  
M. Nearing ◽  
C. Alewell

Abstract. Mountainous soil erosion processes were investigated in the Urseren Valley (Central Switzerland) by means of measurements and simulations. The quantification of soil erosion was performed on hill slope scale (2·20 m) for three different land use types: hayfields, pastures with dwarf shrubs and pastures without dwarf shrubs with three replicates each. Erosion rates during growing season were measured with sediment traps between June 2006 and November 2007. Long-term soil erosion rates were estimated based on Cs- 137 redistribution. In addition, soil moisture and surface flow were recorded during the growing season in the field and compared to model output. We chose the WEPP model (Water Erosion Prediction Project) to simulate soil erosion during the growing season. Model parameters were determined in the field (slope, plant species, fractional vegetation cover, initial saturation level), by laboratory analyses (grain size, organic matter) and by literature study. The WEPP model simulates sheet erosion processes (interrill and splash erosion processes, please note that no rill erosion occurs at our sites). Model output resulted in considerable smaller values than the measured erosion rates with sediment traps for the same period. We attribute the differences to observed random gravity driven erosion of soil conglomerates. The Cs-137 measurements deliver substantially higher mean annual erosion rates, which are most likely connected to snow cover related processes such as snow gliding and avalanche activities.


2020 ◽  
Author(s):  
Izabella Babcsányi ◽  
Nhung Thi Ha Pham ◽  
Péter Balling ◽  
Zalán Tobak ◽  
Andrea Farsang

<p>Copper (Cu) and zinc (Zn) are important micronutrients for vine plants; however, the long-term use of Cu-fungicides and micronutrient fertilizers can lead to their accumulation in the topsoil of vineyards. Water erosion on sloping vineyards transports sediments downslope, a processus that may redistribute micronutrients in the topsoils. Our study aims at assessing the rate of enrichment in Cu and Zn of vineyard topsoils compared to the geochemical background and their downhill transport during rainfall events attached to sediments.</p><p>The study was conducted in 2019 in a 1,8 ha sloping vineyard at Tokaj (mean slope: 8°) and a 0.4 ha plot near Tállya (mean slope: 18°), both in the historical vinegrowing region of Tokaj-Hegyalja (in northern Hungary). The vineyards at Tokaj have been converted to organic farming, where Cu-based fungicides are repeatedly used in a typical dose of 4 kg/ha/year, supplemented with fertilizers containing micronutrients. The soil samples from the top layers (0-10 cm and 10-20 cm) have been collected using a hand auger from the two vineyards and from local forested sites, the latter accounting for the local geochemical background. Additionally, sediment traps have been deployed for collecting eroded sediment samples. The examined soil type is a Regosol at Tokaj with sandy loam texture, while the Cambisol at Tállya displays slightly heavier soil texture (sandy loam/loam). The soils are characterized by a slightly acidic pH(d.w.) of 6.36±0.27 at Tállya and a moderately alkaline pH(d.w.) of 8.03±0.04 at Tokaj. The differing pH is due to the soil forming parent rocks, that are loess at Tokaj and rhyolite at Tállya. The topsoils (0-20 cm) bear a low to medium organic matter (OM) content (1.5±0.5% OM at Tállya and 1.4±0.2% OM at Tokaj) and a low carbonate content at Tállya (3.1±0.2%), while a low to medium carbonate content at Tokaj (4.4±1.5%).</p><p>The micronutrient (Cu, Zn) concentrations have been determined by an inductively coupled plasma-optical emission spectrometer, following microwave-assisted digestion of powdered soil samples in aqua regia (hydrochloric acid:nitric acid = 3:1). At Tállya, our results show a considerable Cu enrichment and a slight Zn enrichment in the topsoil (mean±se: 127±37 mg/kg Cu, 47±4 mg/kg Zn) due to the repeated use of pesticides and fertilizers, compared to a local forested soil displaying 5 mg/kg Cu and 28 mg/kg Zn. The lower Cu enrichment in the vineyard topsoil at Tokaj (49±14 mg/kg in vineyards, 17 mg/kg at the local forested site) is probably due to the more recent plantation of grapevines. The soil-bound Zn at Tokaj also displayed to some degree higher concentrations in the top 20 cm layers in vineyards (64±6 mg/kg) as to the forest soil, exhibiting 41±3 mg/kg Zn. At both sites, eroded sediments tend to display higher Cu and Zn concentrations relative to the vineyard topsoils with mean enrichment factors (sediments/topsoil) of 4.2 (Cu) and 1.4 (Zn). Additionally, we evidenced that soil erosion significantly affects the topsoil Cu concentrations at Tokaj, as higher Cu concentrations have been found downslope, where the eroded sediments accumulate, compared to the erosion bases upstream.</p>


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