• KOREAN JOURNAL OF CROP SCIENCE
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• v.54 no.1
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• pp.61-79
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• 2009

This study is for incompatible element contents of Perilla frutescens and Sesamum indicum from the Keumsan: biotite granite, phyllite and shale areas. In the soils, high elements are shown in the granite and phyllite areas, and in the areas of the Perilla frutescens. Positive correlations are distinctive within the granite for the Perilla frutescens, but the shale for the Sesamum indicum. These relationships can be explained with relative propositions of minerals containing the incompatible element. In the plants, high elements are shown in the shale and the Sesamum indicum are high in the comparisons of the same soil types. The low parts are mainly high. Regardless of the soil types, the lower and upper parts, respectively, are high in the Y, Zr and Rb contents for the Perilla frutescens, but, Ta, Nb, Th and U contents for the Sesamum indicum. Positive correlations are distinctive within plants of the phyllite. Comparing with the soil types, all HFS and Cs contents of the LFS in the plants are low with differences of several to hundred times, but high in the Sr contents with differences of several times. In the comparisons between plants and soil types, Y, Zr, Hf, Ta, Nb, Rb, and Sr of the phyllite and Th, U, Ba and Cs of the shale for the Perilla frutescens as well as Y, Zr, Hf, Rb, Sr, Ba and Cs of the phyllite and Ta, Nb, Th and U of the shale for the Sesamum indicum are chemically similar to the soils. In the comparisons of the each parts for the plant types, differences with the soils are big in the granite.

• Journal of Ginseng Research
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• v.32 no.3
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• pp.194-209
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• 2008

This study is for major element relationships between ginsengs and soils from three representative soil types from Keumsan, shale, phyllite and granite. In the weathered soils, the granite and phylllite are high while the shale are low. The granite show distinctive positive and negative relationships rather than the phyllite and shale. In the field soils, the granite and phyllite are high while the shale are low. Positive relationships are distinctive with the increasing ages, and in the granite. In the ginsengs, high element contents are shown in K and Na of the shale, Mg and Ca of the phyllite, and Al, Mn and Ti of the granite. In the same regions, the 2 and 3 years are mainly low, but high in the 4 year. Positive correlations are distinctive in the 2 and 4 year of the shale, and 3 year of the granite. Comparisons with ginsengs of the same ages from the different areas suggest that the granite show high element contents with the ages. It also suggests that the 2 year of the granite, and 3 and 4 year of the shale and phyllite are high. Relative ratios(weathered/field soils) among the soils suggest that the weathered are generally high, especially in the granite rather than the shale. Relative ratios between field soils and ginsengs(field soils/ginseng) suggest that the soils are higher than the ginsengs, and differences of several hundred times in the Al and Ti, and of several ten times in the Mn are shown between two. Comparisons among the different ages from the same areas suggest that differences of several hundred times in the Al and Ti are shown. It suggests that ginseng contents are significantly different from the field soils in the Al and Ti contents. Comparisons among from the same ages of the different areas suggest that high element differences are shown in Na of the shale, and Mn of the phyllite, while low element differences are found in Mg of the shale, and Al, Mn, and Na of the granite.

• Proceedings of the Korean Society of Organic Agriculture Conference
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• 2009.12a
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• pp.286-286
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• 2009

벼 유기재배시 토양양분공급용으로 이용되고 있는 유기자재(금수강산골드)를 대조로 하고 식물성유기 자재(쌀겨팰렛), 동물성유기자재, 식물성과 동물성이 혼합된 유기자재를 질소 성분량(7kg/10a)을 기준으로 하여 이앙 20일전에 전량 기비로 시비하고 경운한 다음 동진1호를 시험품종으로 하여 2년연속 유기 자재와 벼를 재배하면서 일어나는 토양의 이화학적 특성과 벼 생육 및 특성의 변화를 시기별로 조사하였다. 시험 전 토양의 화학성은 전반적으로 유기물은 높고 인산함량은 매우 낮은 조건의 토양이었다. 관행유기자재(금수강산골드)는 20일경에 50% 무기화율을 보였으나, 식물성자재 40~60일경, 동물성자재와 혼합자재(식물성+동물성)는 60~80일경에 47~52% 무기화 정도를 나타내 식물성 자재의 무기화 속도가약 20일정도 빨랐다. 토양 중의 유기물 잔존함량은 식물성자재 > 혼합자재 > 동물성자재 > 관행 순이었으며, 토양 중의 전 질소 잔존함량의 경우 관행유기자재는 처리초기부터 빠르게 감소하는 특성을 보이나, 식물성자재와 혼합 자재는 시비초기와 거의 비슷한 수준을 유지하였고, 동물성 자재는 서서히 감소되는 경향이었다. 토양 물리성은 액상과 공극율 다소 증가되는 경향이었으며 식물성과 혼합유기자재처리구가 컸으며, 토양 유효 입단 형성력에 있어서도 유사한 경향이었다. 벼 수량 특성은 관행유기자재보다 1년차에는 3~9%의 낮았으나, 2년 연속처리를 할 경우 관행유기자재를 처리할 때와 동일한 생산성을 기대할 수 있었다. PME와 $\beta$-Glucosidase의 효소활성은 관행유기자재 < 식물성자재 < 동물성자재 < 혼합유기자재의 순으로 높은 경향을 볼 수 있었다.

• Korean Journal of Soil Science and Fertilizer
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• v.34 no.6
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• pp.373-379
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• 2001

The weathering rates and change of chemical composition of 6 residual Entisols derived from granite, granite-gneiss, limestone, sandstone, shale, amd basalt in Korea were studied. The chemical composition of each profile with parent rocks were determined using XRF with the physico-chemical properties and the morphology of soils. In the A horizons of all the soils except Euiseong series, the content of clay, organic matter and cation exchange capacity(CEC) showed higher than those of C horizon, but bulk density and pH showed lower than C horizon. Clay content in the soil from sandstone was decrease with soil depth, which may caused by the elluriation. In total element analysis. $SiO_2$ was high in the soil from granite. granite-gneiss, sandstone and compare with basalt and limestone. $Fe_2O_3$ and MgO was high in the soil from basalt, limestone and shale compare with granite. granite-gneiss and sandstone. And ignition loss was particularly high in the soil from basalt and limestone. The rate of element loss was higher in base cations(Ca, K, Mg, Na) than Si, Al, Fe in the soils. The concentrations of $TiO_2$ in the A horizon compare with that of the C horizon was due to resulting from losses of other less stable elements existed. Considering with relative rate of each elements in soils, $SiO_2$ and $Al_2O_3$ which originated from sandstone and granite, granite-gneiss, sandstone, shale, and basalt were lost higher than those from lime tone, but loss of basic cations were more in the soil from limestone which may be rapid weathering of calcite. The magnitude of losses of the overall elements were increased in the order of the soils from sandstone and granite ${\gg}$ limestone and shale) granite-gneiss and basalt.

• Korean Journal of Organic Agriculture
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• v.19 no.2
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• pp.215-228
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• 2011

To establish the organic cultivation of pepper using green manure crops, this work studied the growth characteristics and yield of green manure crops, mineral composition of green manure crops, mineral uptake in shoots of green manure crops, chemical composition in soil of green manure crops, and the growth characteristics and yield of pepper in vinyl house. Shoot dry weight of green manure crops was higher level in Sorghum bicolor and Sorghum than in Crotalaria juncea and Glycine max. Also, the roots were spread deeply into soil in Sorghum bicolor and Sorghum. Density of root-knot nematodes in rhizosphere of green manure crops was significantly more decrease in Crotalaria juncea and Sorghum than in Glycine max and Sorghum bicolor. Total nitrogen and CaO content of green manure crops was significantly higher in Crotalaria juncea and Glycine max than in Sorghum bicolor and Sorghum. $K_2O$ content was significantly higher in Sorghum bicolor and Sorghum than in Crotalaria juncea and Glycine max. MgO content was not significant difference at all green manure crops. Cations content ratio of $K_2O$ : CaO : MgO was 3.4 : 1.4 : 1. Total nitrogen uptake in shoots of green manure crops was high level in Glycine max, Sorghum bicolor and Sorghum compared with in Crotalaria juncea. $K_2O$ and MgO uptake was significantly higher in Sorghum bicolor and Sorghum than in Crotalaria juncea and Glycine max. Value of pH in soil of green manure crops was more increase in Crotalaria juncea and Glycine max than in Sorghum bicolor, Sorghum and control, but after cultivation of pepper pH in soil was recovered with initial soil pH before seeding of green manure crops. EC value in control, green manure crops, and pepper cultivation decreased by 44%, 15~18%, and 38~61% level, respectively, compared with initial soil of green manure crops treatment. K content in soil of control, Crotalaria juncea and Glycine max cultivation was increased by 14%, but the K content in soil of Sorghum bicolor and Sorghum decreased by 24~38%. Cation exchange capacity (CEC) in soil of Crotalaria juncea and Sorghum bicolor decreased by 11%, but CEC in soil of Glycine max, Sorghum and control increased by 11%. Harvest fruit yield was higher in Crotalaria juncea, Glycine max, and Sorghum bicolor cultivation than in control and Sorghum.

• Korean Journal of Soil Science and Fertilizer
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• v.21 no.1
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• pp.31-40
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• 1988

This study was focussed to compare the concentrations of the volatile oil components of flue-cured tobacco grown by two types of nitrogen-ammonium and nitrate-under vinyl mulching. The results were summarized as follows; 1. The content of nicotine was lower and reducing sugars degraded from starch was higher content in $NO_3-N$ application than $NH_4-N$. 2. The concentrations of furfural, benzyl alcohol, and phenethyl alcohol in the cured leaf were not different between $NH_4-N$ and $NO_3-N$ treatments. 3. Some of the important flavour components-linalool, solanone, damascenone, neophytadiene, and oxyolanone + megastigmatriene-one - had much higher concentrations in $NO_3-N$ than $NH_4-N$ application. 4. In conclusion, nitrate nitrogen was more favorable to decrease nicotine and to increase some important flavour components of cured leaf than ammonium nitrogen.

• Asian Journal of Turfgrass Science
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• v.21 no.2
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• pp.113-126
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• 2007

Mineral nutrients and population dynamics of soil microbes in the root zones of zoysiagrass infected by Rhizoctonia solani AG2-2 and that of healthy plants were sampled from ten golf courses using a cup cutter(diameter $10\;cm\;{\times}\;8\;cm$ deep). Analysis of variance(ANOVA) showed significant differences in content of $NO_3$-N(P = 0.05), $NH_4$-N(P = 0.1), and K(P = 0.1) between infected and healthy samples. The content of $NO_3$-N in the soils of large patch was 9.49 mg/kg and that in soil of healthγ plants was 7.02 mg/kg. However, the content of $NH_4$-N in the soil of large patch was 12.02 mg/kg whereas 14.40 mg/kg for the soil under the healthy plants. The content of K in the soil of large patch was lower than that of soil of healthy plants. There was few numbers of Pseudomonas colonies In the soils of large patch compared to that of healthy plants. These results indicated that the content of $NO_3$-N, NH4-N, and K and the microbial population dynamics in root zones correlated to occurrence of large patch.

• Korean Journal of Soil Science and Fertilizer
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• v.28 no.3
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• pp.241-248
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• 1995

This experiment was conducted to obtain basic information for the management of soil and fertilization for plastic-house soil cultivated Khwari green pepper in Dang Jin area of Chung Nam Province. The range of pH with highest frequency for 36 sites investigated was 6.1~6.5, OM 1.6~2.5%, available phosphorous 601~800mg/kg, CEC 12.1~14.0 c mol/kg, clay 16.1~18.0% and below 2.0ds/m for electical conductivity of soil. Fesh fruit weight of green pepper showed very high significant positive correlation with organic matter, clay content and cation exchange capacity, while negaive correlation with electrical conductivity. Electrical conductivity showed highly significant negative correlation with CEC, clay content and organic matter in soil, respectively. To decrease below 2.0 dS/m of electrical conductivity in plastic-house soil, the content of clay and organic matter could be maintained at above 1.8% and 2.3%, respectively.

• The Korean Journal of Pesticide Science
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• v.3 no.2
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• pp.81-85
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• 1999

Concentration change of soil-applied pretilachlor (2-chloro-2',6'-diethyl- N-2-propoxyethyl)-actanilide) was investigated under upland condition with various soil moisture contents ranging from 50 to 80%(water content by weight). Following pretilachlor from each soil solution was extracted by centrifugation using double tubes, its concentration was determined by HPLC. Pretilachlor concentration in the soil solutions were almost the same under various soil moisture conditions. However, the total amount of pretilachlor increased as the soil moisture content increased. With increasing soil moisture content, the bioactivity of soil-applied pretilachlor on inhibiting the growth of Echinochloa ultilis Ohwi et Yabuno and the absorption of $^{14}C$-pretilachlor in its plants were also enhanced. Our results demonstrate that the absorption of pretilachlor in plants varies with soil moisture content and thus the bioactivity of soil-applied pretilachlor on inhibiting plant growth is different under various soil moisture conditions at the same dosage based on air-dried weight.

• Korean Journal of Environmental Agriculture
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• v.4 no.2
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• pp.78-87
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• 1985

To investigate the effects of paper sludge, by-products of paper manufactory, on the chemical properties of paddy soil and growth of paddy rice, paper sludges were applied to the pots at the rates of 300, 600, 900 and 1,200㎏/l0a which were either pread-justed C/N ratio to 30 : 1 or not adjusted. The effects were compared with those of control. Seasonal variations of various forms of soil organic nitrogen, the mineralization of organic nitrogen and the contents of soil minerals were analyzed. The results were summarized as follows: 1) The contents of soil organic nitrogen, especially amino sugar-N and amino acid-N, organic matter, CEC and available $SiO_2$ were increased by application of paper sludge compared with that of control. 2) The mineralizations of organic nitrogen after 6 weeks of incubation at $30^{\circ}C$ were 12. 2, 12.6, 15.1, 9.7 and $15.2^{\circ}C$ in the control, 300㎏/l0a sludge treatment, 300㎏/l0a sludge treatment(C/N ratio adjusted), 600㎏/l0a sludge treatment and 600㎏/l0a sludge treatment(C/N ratio adjusted), respectively. 3) Cu and Pb contents in the soil were in the range of $0{\sim}0.2100$ and $0{\sim}0.0013$ ppm, respectively. Cr and Cu in the soil were not detected at all. There were no differences in the contents of all the heavy metals among all the treatments in the soil.