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determined directly only by these procedures. Rye breads can be very different in shape, colour, flavour, and texture and are also often mixed with wheat flour ( Arendt and Zannini, 2013 ; Sapirstein and Bushuk, 2016 ). This might be one possible reason why
, mechanical stability, good textural and physicochemical properties, high adsorption capacity, high efficiency, fast kinetics, and the ability to regenerate and reuse ( Dotto and Mckay, 2020 ). Many materials, including agriculture products, red mud, clay
; more than 70% of the area has been hazarded due to IEW inundations; half of the area has heavy textured soils with limited infiltration and low permeability conditions
sowing to harvest (mm). Szarvas, Hungary The soil texture was clay loam with an average pH of 7.5, and with a humus content of 2.5%. Its natural water capacity was 39% by volume, half of which is disposable water. Its total salinity in the upper 30 cm
), in the International Mineral and Organic Nitrogen Fertilization Trial (IOSDV), which is a bifactorial long-term experiment that has been running since 1983. In the experimental area, the soil texture is sandy loam and soil type is Eutric Cambisol
be connected to each other, and interactions between them can be analyzed ( Balamurugan et al., 2019 ; Li et al., 2020 ). At the same time in soil testing, tests based on hyperspectral reflectance can detect moisture content, texture (particle size
forest soil with clay stripes) were the following at 0–25 cm depth: loamy sand texture; pH-H 2 O: 8.10; pH-KCl: 7.52; total salt (m m –1 %): <0.02; CaCO 3 (m m –1 %): 4.80; humus (m m –1 %): 1.51%; CEC (cmol c kg –1 ): 10.4 P-621, K-2,918, Ca-16
Talajnedvesség-tartalom mérése földradarral (GPR) és mezőgazdasági alkalmazhatóságának lehetőségei
Soil water content measurements with ground penetrating radar (GPR) and its application possibilities in the agriculture
of bulk density and texture . Journal of Hydrology . 151 . 147 – 157 . JACOBSEN , O.H ., SCHJØNNING , P ., 1994 . Comparison of TDR calibration functions for soil water determination. In: Proceedings of the Symposium Time Domain Reflectometry
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.
