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        검색결과 6

        2.
        2009.12 KCI 등재 서비스 종료(열람 제한)
        This study was to set the guidelines of soil chemical components in order to assure the safety and quality ofthe panax ginseng from physiological disorder. The disorder symptoms appeared on the leaf with yellow spot, atrophy, yel-low-brown spot, also showed red skin and rough skin of the root. Occurrence type of physiological disorder in cultivatedfield divided into two types:type I ‘such as, yellow spot’ consist of single disorder symptom; type II ‘such as, yellow spotand yellow-brown spot’ consist of two or more different disorder symptoms. The individual contribution of soil properties tothe occurrence type was as follows ; The yellow spot was affected by Na>NO3-N>salinity (EC) in soil. The same results wasobserved in red skin. Atrophy was affected by NO3-N>salinity (EC)>Ca>Mg. Rough skin was affected by P2O5>pH>Organic material > K. It showed positive associated to P2O5, pH and K, but negative associated to organic matter. Simulta-neous occurrence of two different disorder, including cases which yellow spot and yellow-brown spot, those were affected byNO3-N > salinity (EC) > Na > Mg. In the case of atrophy plus yellow-brown spot, those also were affected by in the order :NO3-N > salinity (EC) > Ca > Mg > Na. Red-rough skin was affected in the order : salinity (EC) > NO3-N > K > Na. Soilchemical components appear to be related to occurrence of physiological disorder, particularly in salinity (EC) and NO3-N.The salinity (EC) and NO3-N were negative related to plant growth. In addition, exchangeable cation capacity play criticalroles in attributing to complex occurrence of physiological disorder.
        3.
        2009.12 KCI 등재 서비스 종료(열람 제한)
        The purpose of this study was to identify soil physical characteristics as guideline for high yield potential inginseng cultivated field which produced 6 years root. Harvest yields of ginseng to be divided by parent rock was in order ofphyllite and red shale 3.1㎏/3.3㎡ > granite and gneiss·schist 3.0㎏ > basalt 2.6㎏ > porphyry 2.2㎏ in upland and forestsoil. Also, with classified by topography, it was in order of foot slope and alluvial fan 3.2㎏/3.3㎡ > valley 3.0㎏ > low hill2.9㎏ > hill, lave flow and dilluvial terrace 2.8㎏ in survey tilth. Class determination of soil texture, it was in order of sandyloam 3.1㎏/3.3㎡ > loam and silt loam 3.0㎏ > clay loam 2.9㎏ > silt clay loam 2.8㎏ in survey tilth. Slope condition offarming land, in case of sloping (2~7%), it was 3.1㎏/3.3㎡ but deep sloping (15~30%) caused decreasing harvest yield. Indrainage classes (excessively, well and moderately well), there was no significantly different in harvest yields. Relationshipbetween harvest yield and soil series, Production sites as yielding 3.0㎏/3.3㎡ were seven sites, also it was contained 14 soilseries. Production sites as yielding 2.5~3.0㎏/3.3㎡ were eleven sites, it was contained 16 soil series. Production sites asyielding 2.0~2.5㎏/3.3㎡ were 10 sites, it was contained 4 soil series.