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properties on the spatial variability of soil water content: evidence from sensor network data and inverse modeling Vadose Zone Journal . 13 . ( 12 ) 112 . doi: 10.2136/vzj2014.07.0099 Q u

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. , Hou X. , Zha F. ( 2017 ), Seepage analysis of earth dams considering spatial variability of hydraulic parameters . Engineering Geology , 228 , 260 – 269 . [7] Wang

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] Baker J. W. Faber M. H. Liquefaction risk assessment using geostatistics to account for soil spatial variability J

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Csillag, F., Kertész, M. & Kummert, Á. , 1996. Sampling and mapping of heterogeneous surfaces: multi-resolution tiling adjusted to spatial variability. International Journal of Geographical Information Science. 10 .(7) 851

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. BÁRDOSSY, GY. , 2006 . Geologic and geostatistical evaluation of spatial variability . Acta Geologica Hungarica . 49 . 89 – 101 . B OURENNANE

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). [23] Van Hove L. W. A. , Jacobs C. M. J. , Heusinkveld B. G. , Elbers J. A. , van Driel B. L. Holtslag A. A. M. Temporal and spatial variability of urban

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/BWN/Case, (last visited 15 December 2010 ). [17] Cho S. E. Probabilistic analysis of seepage that considers the spatial variability

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A talaj elektromos vezetőképessége és a termőhelyi zónák talajtulajdonságai közötti összefüggések

Correlations between soil conductivity and soil properties of crop management zones

Agrokémia és Talajtan
Authors: Kocsis Mihály, Menyhárt László, Benő András És, and hermann Tamás

. http://ikr.hu/tudastar_gabonaterm_ml.php Melchiori , P. Z . , 2002 . Spatial Variability Of Wheat Yield, Association With Edaphic Parameters And Assessment Of Application Of Nitrogen For Specific Sites. Thesis For Master Of Science Degree . National

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Our data verified the relationship between meteorological factors and the fluctuation of the groundwater level. The rate of evaporation dominantly affected the rise and depth of the groundwater level. It is characteristic for the study site that there is an inverse relationship between the elevation of the groundwater observation wells and the depth of groundwater, and the difference between the levels of groundwater in the separate wells reflected the differences in the elevation between the wells. Our observations refuted our previous assumptions, as in the wells not only the concentration of salts changed but also the chemical type of the water. This can be attributed with great probability to the lateral flow of the groundwater, which is caused by the vertical fluctuation, but can be caused by other geological factors as well. We reached the conclusion that the vertical and sometimes lateral movement of the groundwater affects the development of soils in a given area. It means that the reason behind the mosaic-like appearance of the soil cover of a given area can be searched in the local differences of the chemical composition of the groundwater, which is a major factor of the spatial variability of the salt accumulation of soils. The observations and analytical results point to that the soils of the study site have developed under the effect of fluctuating groundwater and the elevation is a dominant factor of the spatial variability of the soil salt accumulation. The level of groundwater, the flow of groundwater and its composition show relationship with the surface elevation, and their effect is modified by the geological stratification, which results in a variable appearance of soil salt accumulation and native vegetation.

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