. "N, Z(MSM6215648905)" . . "240709" . . . "978-80-89128-90-7" . . . "V\u00DAPOP Bratislava" . "Use of crop growth anomalies for more precise soil map"@en . "Vyu\u017Eit\u00ED r\u016Fstov\u00FDch anom\u00E1li\u00ED porostu ke zp\u0159esn\u011Bn\u00ED p\u016Fdn\u00EDch map"@cs . "Use of crop growth anomalies for more precise soil map"@en . "Diagnostika, klasifik\u00E1cia a mapovanie p\u00F4d" . "growth anomalies; soil map; aerial photographs"@en . . . . . "Pokorn\u00FD, Eduard" . . "Pode\u0161vov\u00E1, Jitka" . "Vyu\u017Eit\u00ED r\u016Fstov\u00FDch anom\u00E1li\u00ED porostu ke zp\u0159esn\u011Bn\u00ED p\u016Fdn\u00EDch map" . "Brtnick\u00FD, Martin" . . "Vyu\u017Eit\u00ED r\u016Fstov\u00FDch anom\u00E1li\u00ED porostu ke zp\u0159esn\u011Bn\u00ED p\u016Fdn\u00EDch map" . "335"^^ . . "Na leteck\u00FDch sn\u00EDmc\u00EDch porost\u016F zem\u011Bd\u011Blsk\u00FDch plodin jsou \u010Dasto velmi dob\u0159e patrn\u00E1 m\u00EDsta s r\u016Fstov\u00FDmi anom\u00E1liemi (jin\u00E9 zabarven\u00ED, hustota porostu, zm\u011Bna doby dozr\u00E1v\u00E1n\u00ED, pol\u00E9h\u00E1n\u00ED obilnin, atd.). Pokud se jedn\u00E1 o plochy s opakovan\u00FDm v\u00FDskytem, oby\u010Dejn\u011B jasn\u011B ohrani\u010Den\u00E9, je d\u016Fvod domn\u00EDvat se, \u017Ee se jedn\u00E1 o m\u00EDsta s odli\u0161n\u00FDmi p\u016Fdn\u00EDmi vlastnostmi, ne\u017E na ostatn\u00EDch \u010D\u00E1stech pozemku. B\u011B\u017En\u011B se tato metoda pou\u017E\u00EDv\u00E1 v nedestruktivn\u00ED archeologii, kde jsou zm\u011Bny p\u016Fdn\u00EDch vlastnost\u00ED zp\u016Fsobeny antropogenn\u00ED \u010Dinnost\u00ED. Z leteck\u00FDch sn\u00EDmk\u016F porost\u016F je\u010Dmene jarn\u00EDho byla v oblasti Hul\u00EDna vytipov\u00E1na m\u00EDsta star\u00FDch \u0159\u00ED\u010Dn\u00EDch ramen \u0159eky Moravy. R\u016Fstov\u00E9 anom\u00E1lie se projevuj\u00ED p\u0159ed\u010Dasn\u00FDm dozr\u00E1v\u00E1n\u00EDm, v n\u011Bkter\u00FDch letech zaschnut\u00EDm porostu. Na pozemc\u00EDch byl proveden pedologick\u00FD pr\u016Fzkum v m\u00EDstech b\u00FDval\u00FDch ramen \u0159eky a mezi nimi. Typologicky jsou p\u016Fdy \u0159azeny k fluvizem\u00EDm glejov\u00FDm. Bylo prok\u00E1z\u00E1no, \u017Ee v m\u00EDstech b\u00FDval\u00E9ho \u0159e\u010Di\u0161t\u011B je nasycen\u00E1 hydraulick\u00E1 vodivost \u0161estkr\u00E1t vy\u0161\u0161\u00ED ne\u017E mimo \u0159e\u010Di\u0161t\u011B. P\u00F3rovitost s hloubkou v\u00FDrazn\u011B roste v \u0159e\u010Di\u0161ti, mimo \u0159e\u010Di\u0161t\u011B je vy\u0161\u0161\u00ED v povrchov\u00FDch horizontech. Z chemick\u00FDch vlastnost\u00ED byla prok\u00E1z\u00E1na vy\u0161\u0161\u00ED kvalita humusu (HK/FK) mezi toky ve v\u0161ech hloubk\u00E1ch. Obsah p\u0159ijateln\u00E9ho fosforu byl vy\u0161\u0161\u00ED mezi toky v hloubce kolem jednoho metru v \u0159e\u010Di\u0161ti. Respira\u010Dn\u00EDmi testy byla zji\u0161t\u011Bna v m\u00EDstech mezi toky vy\u0161\u0161\u00ED respira\u010Dn\u00ED mohutnost, vy\u0161\u0161\u00ED stabilita organick\u00FDch l\u00E1tek a v\u011Bt\u0161\u00ED nedostatek fyziologicky vyu\u017Eiteln\u00E9ho dus\u00EDku. Zji\u0161t\u011Bn\u00E9 rozd\u00EDlnosti p\u016Fdn\u00EDch vlastnost\u00ED jsou b\u011B\u017En\u00FDmi metodami ter\u00E9nn\u00EDho pr\u016Fzkumu, nebo metodami pedometrick\u00FDmi nemapovateln\u00E9. Vyu\u017Eit\u00ED leteck\u00FDch sn\u00EDmk\u016F porost\u016F se jev\u00ED jako velmi dobr\u00FD dopln\u011Bk p\u0159i sestavov\u00E1n\u00ED p\u016Fdn\u00EDch map."@cs . "On the aerial crop photographs there are often very good visible areas with growth anomalies (different colour, canopy density, change of ripening, lodging of cereals, etc.). In the case of repeated occurrence of areas which are usually clearly delineated, there is reason to consider that these sites have different soil properties than the rest of the land. Normally this method is used in non-destructive archaeology where changes in soil properties are caused by anthropogenic activities. From the aerial photographs of spring barley crops old meanders of the River Morava were identified in Hul\u00EDn area. Growth anomalies are manifested by early maturation, in some years by drying crops. The pedological survey was accomplished in areas of former river meanders and between them. Typologically soils are classified as Gleyic Fluvisols. It was demonstrated that in site of a former river bed the saturated hydraulic onductivity is six times higher than outside the bed. Porosity increases significantly with depth in the stream; outside the river channel the porosity is higher in top horizons. From the chemical properties the higher humus quality (HA/FA) was demonstrated in interfluves sites at all soil depths. Available phosphorus content was higher in interfluves sites into one meter depth in the riverbed. By respiratory tests in nterfluves locations there were found increased respiration capacity, higher stability of organic matter and increasing lack of physiologically usable nitrogen. Observed differences in soil properties cannot be mapped by standard field survey methods, or pedometric methods. Using of crop aerial photographs appears to be a very good supplement tool for soil maps compilation."@en . . "Bratislava" . "RIV/25328859:_____/11:#0000640" . "4"^^ . "6"^^ . "[564832582E55]" . . . "2"^^ . "Vyu\u017Eit\u00ED r\u016Fstov\u00FDch anom\u00E1li\u00ED porostu ke zp\u0159esn\u011Bn\u00ED p\u016Fdn\u00EDch map"@cs . . . "Dene\u0161ov\u00E1, Olga" . "RIV/25328859:_____/11:#0000640!RIV12-MZE-25328859" . "Na leteck\u00FDch sn\u00EDmc\u00EDch porost\u016F zem\u011Bd\u011Blsk\u00FDch plodin jsou \u010Dasto velmi dob\u0159e patrn\u00E1 m\u00EDsta s r\u016Fstov\u00FDmi anom\u00E1liemi (jin\u00E9 zabarven\u00ED, hustota porostu, zm\u011Bna doby dozr\u00E1v\u00E1n\u00ED, pol\u00E9h\u00E1n\u00ED obilnin, atd.). Pokud se jedn\u00E1 o plochy s opakovan\u00FDm v\u00FDskytem, oby\u010Dejn\u011B jasn\u011B ohrani\u010Den\u00E9, je d\u016Fvod domn\u00EDvat se, \u017Ee se jedn\u00E1 o m\u00EDsta s odli\u0161n\u00FDmi p\u016Fdn\u00EDmi vlastnostmi, ne\u017E na ostatn\u00EDch \u010D\u00E1stech pozemku. B\u011B\u017En\u011B se tato metoda pou\u017E\u00EDv\u00E1 v nedestruktivn\u00ED archeologii, kde jsou zm\u011Bny p\u016Fdn\u00EDch vlastnost\u00ED zp\u016Fsobeny antropogenn\u00ED \u010Dinnost\u00ED. Z leteck\u00FDch sn\u00EDmk\u016F porost\u016F je\u010Dmene jarn\u00EDho byla v oblasti Hul\u00EDna vytipov\u00E1na m\u00EDsta star\u00FDch \u0159\u00ED\u010Dn\u00EDch ramen \u0159eky Moravy. R\u016Fstov\u00E9 anom\u00E1lie se projevuj\u00ED p\u0159ed\u010Dasn\u00FDm dozr\u00E1v\u00E1n\u00EDm, v n\u011Bkter\u00FDch letech zaschnut\u00EDm porostu. Na pozemc\u00EDch byl proveden pedologick\u00FD pr\u016Fzkum v m\u00EDstech b\u00FDval\u00FDch ramen \u0159eky a mezi nimi. Typologicky jsou p\u016Fdy \u0159azeny k fluvizem\u00EDm glejov\u00FDm. Bylo prok\u00E1z\u00E1no, \u017Ee v m\u00EDstech b\u00FDval\u00E9ho \u0159e\u010Di\u0161t\u011B je nasycen\u00E1 hydraulick\u00E1 vodivost \u0161estkr\u00E1t vy\u0161\u0161\u00ED ne\u017E mimo \u0159e\u010Di\u0161t\u011B. P\u00F3rovitost s hloubkou v\u00FDrazn\u011B roste v \u0159e\u010Di\u0161ti, mimo \u0159e\u010Di\u0161t\u011B je vy\u0161\u0161\u00ED v povrchov\u00FDch horizontech. Z chemick\u00FDch vlastnost\u00ED byla prok\u00E1z\u00E1na vy\u0161\u0161\u00ED kvalita humusu (HK/FK) mezi toky ve v\u0161ech hloubk\u00E1ch. Obsah p\u0159ijateln\u00E9ho fosforu byl vy\u0161\u0161\u00ED mezi toky v hloubce kolem jednoho metru v \u0159e\u010Di\u0161ti. Respira\u010Dn\u00EDmi testy byla zji\u0161t\u011Bna v m\u00EDstech mezi toky vy\u0161\u0161\u00ED respira\u010Dn\u00ED mohutnost, vy\u0161\u0161\u00ED stabilita organick\u00FDch l\u00E1tek a v\u011Bt\u0161\u00ED nedostatek fyziologicky vyu\u017Eiteln\u00E9ho dus\u00EDku. Zji\u0161t\u011Bn\u00E9 rozd\u00EDlnosti p\u016Fdn\u00EDch vlastnost\u00ED jsou b\u011B\u017En\u00FDmi metodami ter\u00E9nn\u00EDho pr\u016Fzkumu, nebo metodami pedometrick\u00FDmi nemapovateln\u00E9. Vyu\u017Eit\u00ED leteck\u00FDch sn\u00EDmk\u016F porost\u016F se jev\u00ED jako velmi dobr\u00FD dopln\u011Bk p\u0159i sestavov\u00E1n\u00ED p\u016Fdn\u00EDch map." .