Pošlji prispevek (e-pošta) Učinki talnega in foliarnega dodajanja železa in cinka na cvetenje in vsebnost eteričnih olj prave kamilice (Chamomilla recutita (L.) Rauschert), gojene v rastlinjaku
Povzetek
Lončni poskus gojenja prave kamilice (Chamomilla recutita (L.) Rauschert) je bil izveden v rastlinjaku z namenom ugotavljanja talnega in foliarnega dodajanja železa (Fe) in cinka (Zn) na njeno cvetenje, pridelek cvetov in produkcijo eteričnih olj na Faculty of Agriculture, University of Tabriz, Iran, leta 2012. Poskus je bil izveden kot popoln naključni poskus z 12obravnavanji in tremi ponovitvami. Obravnavanja so bila: T1: kontrola – brez gnojenja s Fe ali Zn, T2: 30 mg FeSO4.7H2O kg-1 suhih tal, T3: 22 mg ZnSO4.7H2O kg-1 suhih tal, T4: 30 mg FeSO4.7H2O + 22 mg ZnSO4.7H2O kg-1 suhih tal, T5: škropljenje listov z FeSO4.7H2O (3.5 g L-1), T6: škropljenje listov z FeSO4.7H2O (7.0 g L-1), T7: škropljenje listov s ZnSO4.7H2O (2.5 g L-1), T8: škroplenje listov z ZnSO4.7H2O (5.0 g L-1), T9: T5+T7, T10: T5+T8, T11: T6+T7, T12: T6+T8. Škropljenje listov je bilo opravljeno dvakrat v rastni dobi. Rezultati so pokazali, da je talno in foliarno gnojenje z Fe + Zn značilno povečalo število cvetov, pridelek cvetov, vsebnost in pridelek eteričnih olj v primerjavi s kontrolo. Največje število cvetov (477 na rastlino), največji pridelek cvetov (11.6 g na lonec), največja vsebnost eteričnih olj (0.88 %) in največji pridelek eteričnih olj (119 mg na lonec) so bili izmerjeni pri talnem dodajanju Fe + Zn (T4), povečanje je bilo za 58, 68, 21.4 in 105 % glede na kontrolno obravnavanje. Učinek foliarnega dodajanja Fe + Zn (T12) je bil takoj za talnim dodajanjem Fe + Zn (T4), vendar se od njega ni značilno razlikoval. Druga obravnavanja niso dala značilnih odstopanj od kontrole. V splošnem so rezultati pokazali, da lahko tako talno kot foliarno dodajanje Fe + Zn učinkovito poveča ali izboljša količino in kvaliteto pridelka prave kamilice. Uporabo foliarnega dodajanja bi kot poceni način gnojenja še posebej priporočali na območjih , kjer so tla bazična ali apnenčasta.
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DOI: http://dx.doi.org/10.14720/aas.2015.105.1.04
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