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enhances soil properties physicochemically and biologically [ 47 ]. FA (10–40% w/w) amendments improve soil texture, structure, soil electrical conductivity, dry density, water holding capacity, soil microporosity, pH, and coefficient of permeability from 5
diversity of local culture and natural environment and the potential of regional networks [ 11 ]. 2.2 Use the spatial nature of the terrain to extend the boundary One method to get leftover space to connect with the surrounding is to extend the urban texture
used to make coating masses, fillings and cakes ( Hassim and Dian 2017 ). Replacing it is not nearly as easy, especially in the case of chocolate fillings, because the sensory properties of fat-based fillings (texture, mouthfeel, flavors, etc.) are
Meter CR-400 (Minolta Europe GmbH, Germany) with Ø 8 mm aperture. Furthermore, non-destructive texture evaluation was carried out by a purpose-built tabletop acoustic texture measuring system ( Zsom et al., 2016; Zsom-Muha and Felföldi, 2007 ). Samples
containing starch and/or carrageenan and 2.) a dispersed phase of oil. The role of proteins is to stabilize the dispersed phase ( Wijk et al., 2003 ). Thus, firstly the effect of blood plasma and milk proteins can be considered through texture properties. The
blood texture was measured by viscometric approach. If small amount of dry trisodium-citrate powder can inhibit blood coagulation in industrial environment, the water content of blood may be lower before the following processes. Material and methods
for 168 days on the kinetics and gelation process ( Au et al., 2015 ). They found that plasma and granules participate in the irreversible texture change. Wang and his co-authors examined the gelation time of egg yolk at –18 °C. They found that egg
Szélerózió okozta talaj-, humusz- és tápanyag-áthalmozás különbségeinek feltárása különböző szerkezeti adottságú csernozjom talajokon terepi szélcsatorna kísérletek alapján
Exploring the differences in soil, humus and nutrient accumulation caused by wind erosion on chernozem soils with different structural properties by field wind tunnel experiments
Erosion On Surface Soil Texture And Characteristics Of Windblown Sediments . Journal of Geophysical Research-Biogeosciences . 2009. 114 . G02003 . Larney , F. J ., Bullock , M. S ., Janzen , H. H ., Ellert , B. H ., Olson , E. C. S . , 1998
Summary
During the research, we studied the soil conditions in Zala County's forests and examined the effect on the growth of beech forests on these conditions. Data of National Forest Data Base (NFDB) were analysed for investigation. Most of the forests in Zala County are situated less than 150 m above sea level, their location and topography is very diverse. In most of the forests the groundwater level is deeply beneath the surface so the forests can utilize only the amount of precipitation. In accordance with the geological and climatic conditions, Luvisols were formed predominantly, especially the clayic Luvisols and the gleyic Luvisols are the most typical. In addition, there are still Cambisols and stagnic Luvisols as well. In a small percentage, there are forest stands on rendzinic Leptosols, Vertisol, Regosol and Histosol. According to the favourable parent material, forests have got a deep or medium thickness of soil and the typical texture is loam. Based on the research, soil layer thickness and texture had significant impact on the growth of beech forest stands in terms of soil properties.
The Mócs chondrite was studied by optical microscopy, element mapping, as well as scanning electron microscope backscattered electron (SEM—BSE) imaging, in order to gain a better understanding of the thermal metamorphic as well as post-shock annealing evolution and the mineralogical signatures in this meteorite. The studied thin section of Mócs meteorite contains 26 chondrules with a variety of chondrule textures, which are characterized by a blurry rim. The chondrules mostly consist of pyroxene and olivine, whereas feldspars occur only in the recrystallized groundmass, chondrule mesostasis, and mineral melt inside and beyond the shock veins. It was found that the matrix was completely recrystallized. According to the scanning electron microscope and optical microscope observations mentioned above, it can be concluded that the Mócs chondrite is a 6.5 petrographic type.
