• Korean Journal of Soil Science and Fertilizer
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• v.34 no.4
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• pp.278-283
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• 2001

The overall objective of this research was to show a NIR soil analyzer assessing soil fertility by measuring soil properties rapidly. A total of 140 soil samples were used to obtain calibrations and validation estimating soil properties. The soil samples were ground to pass 0.2mm sieve openings. Partial least square regression analysis was used to develop a calibration for soil analysis. The results indicated that NIR soil analyzer could be used as a routine method for quantitatively determining pH, OM, total nitrogen, CEC, extractable Ca, Mg, K, available $SiO_2$ and soil moisture simultaneously within one minute. Therefore, the NIR soil analyzer may be suitable for quick estimation of soil fertility estimation in fertilizer assessments.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 1996.11a
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• pp.140-143
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• 1996

산성강하물이 산림토양에 미치는 영향을 조사하기 위하여 오염이 우려되는 공단지역(울산, 여천)과 대도시지역(서울, 부산), 그리고 비오염지역인 대조지역(평창, 삼천포)을 대상으로 이들 지역의 산림토양의 특성을 조사하였다. 또한, 이들지역 각각을 대표할 수 있는 산림토양에 인공산성비를 유출시켜 토양의 화학적 성질의 변화를 조사한 결과는 다음과 같다. - 조사지역별 토성분포는 일정한 경향을 보이지 않았으며, 전체 조사지역 토성은 양토(29.0%), 식양토(22.9%), 사양토(18.3%) 3종류가 분포율이 높았고, 이들이 전체의 70.2%를 차지하였다. - 조사지역 전체 산림토양 표토의 pH($H_2O$)는 4.41~5.14 범위로 평균 4.49이고, 심토의 pH($H_2O$)는 4.54 ~ 5.22 범위로 평균 4.69이었다. 지역별로 보면 공단지역(4.44) < 대도시지역(4.57) < 대조지역(5.08) 순서로 토양 pH가 낮은 경향을 나타냈다. - 염기포화도는 3.07 ~ 21.83% 범위이고, 평균값은 7.71%이었다. 지역별 비교에서는 대조지역(19.14%) > 공단지역(6.54%) > 대도시지역(5.60%) 순서로 높은 경향을 보였다. - 치환성 Al 함량은 2.13 ~ 5.59cmol(+)/kg 범위이고 평균 4.62cmol(+)/kg이었다. 지역별 비교에서는 대조지역(2.34) < 대도시지역(3.23) < 공단지역(5.20) 순서로 낮은 경향을 나타냈다. - 4종의 인공산성우(pH 2.0, 3.0, 4.0 및 5.6)를 산림토양에 유출시킨 결과 인공산성우의 유출량이 증가함에 따라 토양유출액의 pH 감소, 토양염기의 유실이 지속적으로 나타났고, AL과 Mn의 용탈량이 증가하는 경향을 나타내었는데, 이러한 현상은 pH 3.0 인공산성우 유출시에 시작되어 pH 2.0에서 뚜렸하였다. - 인공산성우 토양유출 실험결과 울산, 남산 및 평창토양은 H 부하량의 증가에 따른 치환성염기 및 Al과 Mn의 용탈양상은 Sigmoid curve인 y = a/{1+exp(-c+bx)} 모델식에 따랐다.

• Korean Journal of Soil Science and Fertilizer
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• v.45 no.2
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• pp.253-259
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• 2012

Disposal of high amount of coal combustion by-products, such as fly ash and bottom ash, is of a great concern to the country, due to the huge treatment cost and land requirement. On the other hand, those coal-ash wastes are considered to have desirable characteristics that may improve physical, chemical, and biological properties of soils. Especially, compared with fly ash, bottom ash has a larger particle size, porous surface area, and usable amount of micronutrients. In the present study, we examined bottom as a soil amendment for mitigating $CO_2$ emission and enhancing carbon sequestration in soils fertilized with organic matter (hairy vetch, green barely, and oil cake fertilizer). Through laboratory incubation, $CO_2$ released from the soil was quantitatively and periodically monitored with an enforced-aeration and high-temperature respirometer. We observed that amendment of bottom ash led to a marked reduction in $CO_2$ emission rate and cumulative amount of $CO_2$ released, which was generally proportional to the amount of bottom ash applied. We also found that the temporal patterns of $CO_2$ emission and C sequestration effects were partially dependent on the relative of proportion labile carbon and C/N ratio of the organic matter. Our results strongly suggest that amendment of bottom ash has potential benefits for fixing labile carbon as more stable soil organic matter, unless the bottom ash contains toxic levels of heavy metals or other contaminants.

• Proceedings of the Korean Society for Applied Microbiology Conference
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• 1978.04a
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• pp.98.5-99
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• 1978

항생물질과 RNA 분해효소를 동시에 생산하는 방선균의 한 균주를 토양으로부터 분리하여 이 균주가 생산하는 RNA 분해효소의 물리화학적 성질 및 분해산물에 대해 검토하였다. 효소반응의 최적 pH 및 온도는 명명 pH 5.6과 $50^{\circ}C이었다.$ $37^{\circ}C$ 에서 90분간 열처리 시켰을 때, 이 효소의 활성은 비교적 안정하였지마는 $50^{\circ}C$ 에서 90분간 열처리 시켰을 때는 효소활성이 심하게 저하되었다. 이 효소의 활성은 $Ba^{2+}$ 에 의하여 50% 정도의 저해 작용을 나타내었지만 EDTA에 의해서는 저해되지 않았다. 이 효소에 의한 RNA분해로 이 효소가 대사산물로서 guanosine, adenosine과 밝혀지지 않은 두 가지의 핵산관연물질을 생산함을 알 수 있었다. 제2보에서는 ENase의 효소학적 성질을 검토하였으며 이후 항생물질 측면에서 검토할 예정이다.

• Plant Journal
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• v.12 no.1
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• pp.37-43
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• 2016

The corrosivity evaluations on soil surrounding the buried steel piles under manufacturing plants. It was proven that the soil structure of this sample area is composed of several soil layers, and that each layer show the different corrosivity. The predicted average corrosion rates of some layers are about 0.33mm/y, which is over than the general corrosion rate, 0.01-0.02mm/y.

• Korean Journal of Soil Science and Fertilizer
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• v.21 no.3
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• pp.241-245
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• 1988

The characteristics of some hillside soils in Yeongnam area were investigated to obtain the basic informations for reclamation. Some physico-chemical properties of the soils were discussed with erodibility factor (K) and aggregate stability. The domain clay mineral of soils was identified as Kaoline. Their exchangeable AI, Fe contents were high, and phosphate adsorption coefficients were ranged from 246 to 551 p mg/100g. The improvement of their physico-chemical properties is required in advance to reclaim at those soils.

• Journal of Soil and Groundwater Environment
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• v.13 no.2
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• pp.21-29
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• 2008

Sorption and desorption processes play an important role in the transport and fate of organic contaminants in subsurface system. In this study, sorption and desorption characteristics of atrazine in 7 soils selected at the Gwangju area were investigated. Soil organic carbon contents ranged from 0.42 to 2.82%. Sorption and desorption experiments were performed in batch slurries. Sorption distribution coefficient ($K_d$) of atrazine were ranged from 0.48 to 3.26 l/kg and $K_d$ value increased with increasing organic carbon contents except of Kyongbang and Youngdong soils. Single desorption data were analyzed by the three-site desorption model including equilibrium, non-equilibrium and non-desorbable site. Non-desorbable site fractions of atrazine in all soils were enumerated and non-desorbable atrazine was observed in seriesdilution desorption experiment. Sorption/desorption hysteresis was also observed in the series-dilution desorption experiment.

• Korean Journal of Agricultural Science
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• v.18 no.1
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• pp.74-79
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• 1991

In order to use of new organic matter source, soil samples collected from paddy, upland and orchard treated with kraft and paper board mill sludge were analysed comparing with non-treated soil in view of some soil properties, soil microorganisms and soil enzyme activities. Also, the value of fertilizer was estimated with kraft and paper board mill sludge. 1. Paper mill sludge showed more than 55% of organic matter content, and higher total nitrogen and phosphorus, and CEC. 2. Soils treated with kraft sludge were higher contents than non-treated 2.5-3 for organic matter, 1.5-2 for total-nitrogen, 2 for $NO_3$-N, 1.5 for phosphorus and 1.4 times for CEC. Also, 12-1.9 for bacteria and 3 times for fungi, and 1.4-1.5 of cellulase, 1.5-1.8 of phosphatase and 1.5-1.8 times of urease activities. 3. Organic matter contents, number of fungi, and activities of cellulase and phosphatase in soil treated with paper board sludge were 1.4-22, 2.4, 1.5-1.6 and 1.3-1.4 times higher than non-treated soil, respectively. 4. Paper mill sludge was evaluated as a good organic matter source to increase of soil organic matter, CEC, inorganic components, soil microbes and enzyme activities.

• Journal of the Korean Geographical Society
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• v.44 no.2
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• pp.122-145
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• 2009

Terrain parameters calculated from digital elevation models (DEM) have become increasingly important in current spatially distributed models of earth surface processes. This paper investigated how the ability of upslope area for predicting the spatial distribution of soil properties varies depending on the selection of spatial resolutions of DEM and algorithms. Four soil attributes from eight soil-terrain data sets collected from different environments were used. Five different methods of calculating upslope area were first compared for their dependency on different grid sizes of DEM. Multiple flow algorithms produced the highest correlation coefficients for most soil attributes and the lowest variations amongst different DEM resolutions and soil attributes. The high correlation coefficient remained unchanged at resolutions from 15 m to 50 m. Considering decreasing topographical details with increasing grid size, we suggest that the size of 15-30 m may be most suitable for soil-landscape analysis purposes in our study areas.

• Journal of Korean Society of Forest Science
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• v.76 no.2
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• pp.127-137
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• 1987

This study was conducted to examine the effects of trampling on the changes in soil and vegetation around the trails. The study areas were established both on the trails and in the forested areas located in Ui and Jeongnung valleys at Pukhansan National Park. Soil core sampling, measurements of vegetations and counts of persons visited per hour were done during the period from April 6 to October 9, 1986. The physical properties of soils became better with increasing distances from the trail, and the best conditions were observed in the forested areas. The differences were not significant among the zones within the trailside. More number of individuals and basal area (or coverage) in woody plants were observed in the forested areas than at trailsides. For the herb layer, however, more number of individuals and coverage were shown at the trailside. In the Ui valley, the quantitative measures of herbaceous plants decreased as the bulk density and penetration resistance increased. In the Jeongnung valley, however, only bulk density was negatively related to the quantitative measures. The fact that there were poor relations between soil factors and quantitative measures of herbaceous plants in Jeongnung valley might be influenced by other factors rather than soil compaction. Thus, more research would be needed to understand the critical factors affecting the vegetational changes in recreation areas.