"75;83" . . "Aplikace pedotransferov\u00FDch funkc\u00ED p\u0159i odhadu hydrofyzik\u00E1ln\u00EDch charakteristik p\u016Fdy"@cs . "Nov\u00E9 Hrady" . "P(GA103/02/0971), Z(MSM6046070901)" . "Neuvedeno, 0" . "Matula, Svatopluk" . "P\u016Fdn\u00ED hydraulick\u00E9 vlastnosti se pou\u017E\u00EDvaj\u00ED jako vstupn\u00ED data pro simulaci transportu vody a roztok\u016F v p\u016Fdn\u00EDm profilu. Velmi d\u016Fle\u017Eitou charakteristikou je reten\u010Dn\u00ED \u010D\u00E1ra p\u016Fdn\u00ED vlhkosti a hydraulick\u00E1 vodivost. Reten\u010Dn\u00ED \u010D\u00E1ra p\u016Fdn\u00ED vlhkosti p\u0159edstavuje mno\u017Estv\u00ED vody, kter\u00E9 je zadr\u017Eov\u00E1no p\u016Fdou za podm\u00EDnek rovnov\u00E1\u017En\u00FDch stav\u016F a je unik\u00E1tn\u00ED pro ka\u017Edou p\u016Fdu. Laboratorn\u00ED stanoven\u00ED reten\u010Dn\u00ED \u010D\u00E1ry je pracn\u00E9, \u010Dasov\u011B n\u00E1ro\u010Dn\u00E9 a \u010Dasto nejsou pot\u0159ebn\u00E1 data k dispozici. Proto se rozv\u00EDj\u00ED pou\u017E\u00EDv\u00E1n\u00ED model\u016F odhadu reten\u010Dn\u00ED \u010D\u00E1ry. Na z\u00E1klad\u011B znalosti l\u00E9pe dostupn\u00FDch p\u016Fdn\u00EDch vlastnost\u00ED, jako je zrnitost, obsah organick\u00E9 hmoty, p\u016Fdn\u00ED struktura a objemov\u00E1 hmotnost. Bouma, 1989 nazval takov\u00E9to modely pedotransferov\u00FDmi funkcemi. Pr\u00E1ce navazuje na v\u00FDsledky evropsk\u00E9ho \u0159e\u0161en\u00ED: W\u00F6sten et al. 1998, W\u00F6sten et al. 1999 a dal\u0161\u00ED. Pou\u017Eit\u00E1 metodologie pro zpracov\u00E1n\u00ED dat byla stejn\u00E1 jako pou\u017Eil W\u00F6sten et al. 1998 pro tzv. kontinu\u00E1ln\u00ED pedotransferov\u00E9 funkce. Tyto funkce byly testov\u00E1ny na datech z n\u00E1sleduj\u00EDc\u00EDch lokalit \u010Cesk\u00E9 republiky: Cerhovice"@cs . "Pedotransfer Function Application for Estimation of Soil Hydrophysical Properties"@en . "9"^^ . . . "Pedotransfer Function Application for Estimation of Soil Hydrophysical Properties"@en . . "2"^^ . . "P\u016Fdn\u00ED hydraulick\u00E9 vlastnosti se pou\u017E\u00EDvaj\u00ED jako vstupn\u00ED data pro simulaci transportu vody a roztok\u016F v p\u016Fdn\u00EDm profilu. Velmi d\u016Fle\u017Eitou charakteristikou je reten\u010Dn\u00ED \u010D\u00E1ra p\u016Fdn\u00ED vlhkosti a hydraulick\u00E1 vodivost. Reten\u010Dn\u00ED \u010D\u00E1ra p\u016Fdn\u00ED vlhkosti p\u0159edstavuje mno\u017Estv\u00ED vody, kter\u00E9 je zadr\u017Eov\u00E1no p\u016Fdou za podm\u00EDnek rovnov\u00E1\u017En\u00FDch stav\u016F a je unik\u00E1tn\u00ED pro ka\u017Edou p\u016Fdu. Laboratorn\u00ED stanoven\u00ED reten\u010Dn\u00ED \u010D\u00E1ry je pracn\u00E9, \u010Dasov\u011B n\u00E1ro\u010Dn\u00E9 a \u010Dasto nejsou pot\u0159ebn\u00E1 data k dispozici. Proto se rozv\u00EDj\u00ED pou\u017E\u00EDv\u00E1n\u00ED model\u016F odhadu reten\u010Dn\u00ED \u010D\u00E1ry. Na z\u00E1klad\u011B znalosti l\u00E9pe dostupn\u00FDch p\u016Fdn\u00EDch vlastnost\u00ED, jako je zrnitost, obsah organick\u00E9 hmoty, p\u016Fdn\u00ED struktura a objemov\u00E1 hmotnost. Bouma, 1989 nazval takov\u00E9to modely pedotransferov\u00FDmi funkcemi. Pr\u00E1ce navazuje na v\u00FDsledky evropsk\u00E9ho \u0159e\u0161en\u00ED: W\u00F6sten et al. 1998, W\u00F6sten et al. 1999 a dal\u0161\u00ED. Pou\u017Eit\u00E1 metodologie pro zpracov\u00E1n\u00ED dat byla stejn\u00E1 jako pou\u017Eil W\u00F6sten et al. 1998 pro tzv. kontinu\u00E1ln\u00ED pedotransferov\u00E9 funkce. Tyto funkce byly testov\u00E1ny na datech z n\u00E1sleduj\u00EDc\u00EDch lokalit \u010Cesk\u00E9 republiky: Cerhovice" . . . "41210" . "2"^^ . "\u0160pongrov\u00E1, Kamila" . . "Ochrana a vyu\u017Eit\u00ED p\u016Fdy v podhorsk\u00FDch oblastech - Land use and soil protection in submountain area" . . "512683" . . "80-7040-818-9" . "[92C3791068D4]" . . . "RIV/60460709:41210/05:11263" . . "soil moisture retention curve, multiple linear regression, pedotransfer functions"@en . "\u010Cesk\u00E9 Bud\u011Bjovice" . . "Aplikace pedotransferov\u00FDch funkc\u00ED p\u0159i odhadu hydrofyzik\u00E1ln\u00EDch charakteristik p\u016Fdy" . "Soil hydraulic properties are needed as input to describe and simulate transport of water and solutes in the soil profile. The most important characteristics are the soil moisture retention curve (SMRC)0 (h) and hydraulic conductivity. SMRC represents the amount of water remaining in the soil under equilibrium conditions and is unique for each soil. The measurement of the SMRC is labour s and time consuming and sometimes there are not enough dta available. The SMRC esmination models have been used extensively. more available soil properties, such as calculations. Bouma, 1989 called these models pedontransfer functions. This preliminary study is based on the following European works: W\u00F6sten et al. 1998, W\u00F6sten et al., 1999 and others. Pedotransfer functions derived by W\u00F6sten et all, 1998 were used in the first part of the study. In the second part own pedotransfer functions were derived for localities with available data. The methodology of data processing ws the same as used in W\u00F6sten et al., 1998 fo"@en . "Aplikace pedotransferov\u00FDch funkc\u00ED p\u0159i odhadu hydrofyzik\u00E1ln\u00EDch charakteristik p\u016Fdy"@cs . "Jiho\u010Desk\u00E1 univerzita v \u010Cesk\u00FDch Bud\u011Bjovic\u00EDch. Zem\u011Bd\u011Blsk\u00E1 fakulta" . "RIV/60460709:41210/05:11263!RIV06-GA0-41210___" . . "2005-09-01+02:00"^^ . . . "Aplikace pedotransferov\u00FDch funkc\u00ED p\u0159i odhadu hydrofyzik\u00E1ln\u00EDch charakteristik p\u016Fdy" . . .