• Proceedings of the Zoological Society Korea Conference
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• 1996.10a
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• pp.117.2-117
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• 1996

• Proceedings of the Korean Environmental Sciences Society Conference
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• 1999.10a
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• pp.171-172
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• 1999

• Korean Journal of Soil Science and Fertilizer
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• v.39 no.1
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• pp.29-37
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• 2006

In remediation of the contaminated soil, it requires to select at least more than two remediation technologies depending on the fate and transport phenomena through complicated reactions in soil matrix. Therefore, methodologies related to develop the integrated remediation technology were reviewed for agricultural soils contaminated with heavy metals. Pneumatic fracturing is necessary to implement deficiency because soil washing is not effective to remove heavy metals in the subsurface soil. But it needs to evaluate the characteristics such as essential data and factors of designated technology in order to effectively apply them in the site. In the remediation site, the important soil physical and chemical factors to be considered are hydrology, porosity, soil texture and structure, types and concentrations of the contaminants, and fate and its transport properties. However, the integrated technology can be restrictive by advective flux in the area which remediation is highly effective although both soil washing and pneumatic fracturing were applied simultaneously in the site. Therefore, we need to understand flow pathways of the target contaminants in the subsurface soils, that includes kinetic desorption and flux, predictive simulation modeling, and complicated reaction in heterogenous soil.

• Journal of Korean Society of Forest Science
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• v.84 no.2
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• pp.178-185
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• 1995

Air pollution effects on soil chemical properties, denitrifying and sulfur-reducing bacteria and lichens were examined around the Yeochun industrial estate. Soil samples were collected from mountain and/or mountain edges around the Namhae Chemical Corp., which is located at the southern edge of the estate, and sampled plots which were selected at 2km, 4km, 6km, 8km, and 10km apart from the industrial estate. The forest soils around the industrial estate could be classified into the Reddish yellow forest soil group, but soil pH was quite lower than the soils of the group. Because of the extremely low soil pH, microbial activity related to mineralization of organic matter was expected to be very low even though C/N ratio ranged from 15 to 20. As a result, soil organic matter and total nitrogen in soil were relatively high compared to the soils of the group. In general, soil chemical properties around the industrial estate up to 4km apart from the estate were significantly different from the rest(more than 6km apart from the estate) possibly due to air pollution. However, denitrifying bacteria and sulfur-reducing bacteria did not show significant differences in colony forming units by the distances from the industrial estate. By the way, lichens showed distinct differences in frequencies and coverages by the distances from the industrial estate possibly due to air pollution. The corticolous lichens showed more sensitive response to the air pollution compared to the saxicolous lichens.

• Korean Journal of Heritage: History & Science
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• v.45 no.4
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• pp.114-125
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• 2012

The purpose of this study is to analysis chromaticity, granulometry, main chemical composition and mineral crystal structure of wall soils excavated from Poongnatoseong Earthen Castle using color reader, XRD, particla size analyzer. The analysed soils of Poongnatoseong Earthen Castle were yellowish brown and isabella. All samples were sands or sands including silty soil(SW~SC) and showed similar granulometry, chemical composition and mineral crystal structure, which were characteristics of construction materials suitable for modern road or airstrip. As resulting in comparison with 4 factors from chromaticity, granulometry, main chemical composition and mineral crystal structure, we decided that the control soils(PNS) near by Poongnatoseong Earthen Castle were not to be used for the castle wall construction We presumed that there was a huge soil distribution area for the wall construction around Poongnatoseong Earthen Castle. For further study, we will make a comparison analysis all kinds of soil characteristics. And then we can understand correctly about wall soils producing area, construction method, repair method and time of Poongnatoseong Earthen Castle.

• Proceedings of the Korean Society for Bio-Environment Control Conference
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• 1994.05a
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• pp.34-54
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• 1994

1. 고형배지특성 (1) 물리화학성 토양재배에서는 토양이 갖고 있는 다양한 완충작용, 즉 보수, 통기성, 비료성분의 보유능력이 대단히 높기 때문에 연작장해가 없는 한 작물생산에서 안정적 생산이 가능하다. 반면에 양액재배에서는 이러한 완충능을 기대하기가 어렵다. 특히 배지에 따른 물리화학성의 차이가 있고 이들 배지의 활용을 근본적으로 근권환경의 제어라는 측면에서 기존의 토양재배보다 높은 생산성과 고품질을 요구하고 있는 실정이기 때문에 배지에 따른 적정 근권환경제어가 필요하다. (중략)

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.28-30
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• 2007

• Korean Journal of Soil Science and Fertilizer
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• v.44 no.5
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• pp.709-716
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• 2011

In order to collect basic data of soil environment in the Vicinity of King Sejong Station, King George Island, Antarctica, the physico-chemical characteristics of soils were investigated. Soil samples were collected in Barton Peninsula from 13 sites according to direction from the Sejong Cape. Soils from 13 sites were divided into three groups. The sand percentage of soils were much higher as above 90% than silt and clay percentages of soils at the all sites. Soil texture was classified sandy (10 sites) and loamy sand (3 sites). In distribution characteristics at different soil particles according to direction, large particles ($>500{\mu}m$) were higher in the order of Group 1 (Marian cove coast regions) > Group 2 (Inland regions) > Group 3 (Maxwell bay coast regions). On the other hand, small particles ($<355{\mu}m$) were higher in the order of Group 3 > Group 2 > Group 1. Chemical characteristic of soils showed significant differences at different areas. pH ranged 4.5-6.7, showing it was slightly acid and EC ranged $0.06-0.16dS\;m^{-1}$. T-N, OM and T-C contents were high at #6, #8, #12 and #13 sites. T-P and P2O5 contents were high at #9 and #12 sites. The results of this study will be helpful to understand soil environment in the Antarctic Peninsula and surrounding islands.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2006.04a
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• pp.298-301
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• 2006

지하수 장해를 사전에 방지하고 지하수의 유동특성과 배경수질을 파악하기 위해 설치된 국가 지하수관측망에서는 지하수위, 전기전도도, 수온 항목을 주기적으로 측정하고 있으며 아울러 연 2회 생활용수 기준의 수질검사를 실시하고 있다. 이들 측정항목의 시간적 변화를 고찰함으로써 해당 지하수계의 이상 징후를 효과적으로 감지할 수 있다. 하지만, 이들 측정항목 만으로는 지하수의 수리화학적 환경을 제대로 파악하기가 어려우며, 따라서 지하수 수질 장해가 인지되었을 경우 그 원인을 효과적으로 규명하기가 쉽지 않다. 지하수 수질 장해는 인위적인 오염 외에도 지질 조건과 관련한 자연적 과정에 의해서도 빈번히 일어난다. 지하수 수질 장해의 원인과 지하수의 수질 변화 경향을 파악하기 위해서는 관측 항목에 추가하여 양/음이온 분석자료의 주기적 취득과 수리 지구화학적 해석이 필요하다. 금번 발표에서는 국가 지하수 관측망의 장기 관측 결과 지하수 수질 장해 우려지역으로 제안된 5개 지역의 수리지구화학 조사연구 사례를 소개한다. 관측망 관정 외에 주변 지역 지하수에 대한 양/음이온 분석을 수행하고 수리지구화학 해석을 수행함으로써 지하수 수질장해의 원인을 규명할 수 있었다.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2004.04a
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• pp.272-276
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• 2004

화강암에 대한 화학적 풍화특성과 풍화 정도의 정량적으로 표현하기 위한 방법으로 조사지역의 지형자료에 기초한 습윤지수(wetness indes)를 산정하였으며, 중화속도 및 등급을 산정하였다. 습윤지수는 지형 고도를 이용하여 2-5m 크기의 격자로 구성 된 수치고도모형을 작성하여 계산하였으며 풍화속도와 등급은 Profile model을 이용하였다. 연구대상지역은 마산지역과 서부산지역으로 집수지형을 지시하는 습윤지수의 분포는 마산지역에서 다소 높은 지수 값을 보인다. 임계부하량(critical loads)에 의한 풍화등급은 마산 가포동 지역과 서부산 견마도 지역은 각각 3등급과 4등급에 해당하여 견마도 일원에서 높은 풍화 정도를 지시한다. 이와 같은 결과는 동일한 화강암 분포지의 경우에도 구성 광물의 비율과 기온과 강수량과 같은 지역적인 특성에 따라 상이한 풍화 경향이 나타남을 지시한다.