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Description
| - Agricultural lands in foothill zones on acid crystalline rocks in Central Europe can be an important source of diffused nitrate pollution of waters. The decisive factors of soil water regime on texturally heavier sites, usually classified as pseudogleys (planosols), are soil macropores and the parent rock heterogeneity. Typical phenomena observed during soil moisture and water quality monitoring are the local non-equilibrium of soil water, different reactions of individual sensors to precipitation and irrigation, the variability of soil hydraulic conductivity in both space and time, and the variability and intermittent character of water percolation in lysimeters. This paper attempts to explain the observed spatial variability of soil moisture suction fields in a statistical way.
- Agricultural lands in foothill zones on acid crystalline rocks in Central Europe can be an important source of diffused nitrate pollution of waters. The decisive factors of soil water regime on texturally heavier sites, usually classified as pseudogleys (planosols), are soil macropores and the parent rock heterogeneity. Typical phenomena observed during soil moisture and water quality monitoring are the local non-equilibrium of soil water, different reactions of individual sensors to precipitation and irrigation, the variability of soil hydraulic conductivity in both space and time, and the variability and intermittent character of water percolation in lysimeters. This paper attempts to explain the observed spatial variability of soil moisture suction fields in a statistical way. (en)
- Znečištění vodních zdrojů u zemědělských ploch dusičnany může mít významné následky. Dalším nepříznivý faktorem jsou texturně těžší půdy, klasifikované jako pseudogleje, půdní makropóry a heterogenita matečné horniny. Typickým průvodním jevem vodního půdního režimu je lokální nerovnováha půdních sacích tlaků, rozdílné reakce tlakových čidel na srážku nebo závlahu, variabilita hydraulické vodivosti v prostoru a času, nespojitý průsak vody do lyzimetrů. Náš příspěvek chce pomocí statistiky objasnit měřenou prostorovou variabilitu půdních sacích tlaků. (cs)
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Title
| - Quantifying the joint effect of soil macropores and soil heterogeneity through the statistics of soil moisture heterogeneity and a model of dual permeability medium
- Quantifying the joint effect of soil macropores and soil heterogeneity through the statistics of soil moisture heterogeneity and a model of dual permeability medium (en)
- Kvantifikace vlivu makropórů a půdní heterogenity pomocí statistické analýzy půdní vlhkosti a modelem zahrnujícím koncept duální pórovistosti (cs)
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skos:prefLabel
| - Quantifying the joint effect of soil macropores and soil heterogeneity through the statistics of soil moisture heterogeneity and a model of dual permeability medium
- Quantifying the joint effect of soil macropores and soil heterogeneity through the statistics of soil moisture heterogeneity and a model of dual permeability medium (en)
- Kvantifikace vlivu makropórů a půdní heterogenity pomocí statistické analýzy půdní vlhkosti a modelem zahrnujícím koncept duální pórovistosti (cs)
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skos:notation
| - RIV/68407700:21110/04:01105138!RIV/2005/GA0/211105/N
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http://linked.open...avai/riv/aktivita
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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| - RIV/68407700:21110/04:01105138
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http://linked.open...in/vavai/riv/obor
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http://linked.open...UplatneniVysledku
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http://linked.open...iv/tvurceVysledku
| - Císlerová, Milena
- Dohnal, Michal
- Dušek, Jaromír
- Vogel, Tomáš
- Štekauerová, V.
- Doležal, F.
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https://schema.org/isbn
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http://localhost/t...ganizacniJednotka
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