• 한국대기환경학회지
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• 제11권2호
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• pp.191-198
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• 1995

In order to evaluate the distribution and behaviour of atmospheric particulate metals in high-altitude area, we collected 22 aerosol samples using a high volume air sampler at Soback Mt. Meteorological Observation Station from Jan. to Nov. 1993 and analysed for metals (Al, Fe, Mg, Na, Ca, Mn, Co, Ni, Cu, Zn, Cd, and Pb) with ICP/AES and ICP/MS. Although sampling site is located in high-altitude and far from local sources of atmospheric pollutants, enrichments of metals are 2 times higher than those of western coastal reural area. This fact may imply that of metallic pollutants in the coastal rural site were came from further western side (e.g. China), atmospheric metals in this study area contain the signal of metropolitan cities located in the main wind direction (NNW). Sea salts are negligible in the aerosol particle population because reference elements of sea salts (Na, Mg) are all originated from soil particles. The contents of soil particles in aerosols are highest in spring and lowest in winter. Atmospheric enriched elements (Ni, Cu, Zn, Cd and Pb) are diluted with soil particles, especially during the yellow sand period. The results of factor analysis suggest possibility of interpreting their chemical significance in terms of sources (soil, pollutants) and gas-particle conversion processes (formation of ammonium sulfates, ammonium nitrates and/or their mixtures).

• 한국환경복원기술학회지
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• 제14권6호
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• pp.87-95
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• 2011

This study investigates Youl Chon Industrial Complex 1 by dividing into three regions : the drainage site, the area inside the complex, and the seaside. Then each region was subdivided into three areas resulting in a total of nine areas for soil sampling and analysis. After analyzing the physical and chemical properties of the soil, all nine area's pH and EC readings indicated that the soil condition is not suitable for vegetation growth (according to the previous study, the pH level was 5.8 and EC was 2.0dS/m). Therefore, for Youl Chon Industrial Complex 1 to become green, the neutralization and reduction of pH and EC level is needed; first, vegetation through dredging soil, and second, introduction of halophytes is suggested. This study finds out that vertical changes in physical and chemical properties of soils in reclaimed sites are very variable and the result depends on surrounding environments, so it suggested the basic data for building vegetation or reclaimed sites. However, the additional study aiming at various reclaimed sites is required as this study was conducted only to limited areas, and this study has left monitoring analysis as the follow-up task to check the relations between a plant community and soils.

• 한국자원식물학회지
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• 제4권2호
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• pp.51-58
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• 1991

With the soil samples collected from 33 locations in Kwangju area, the physiochemical properties of soil and soil microorganisms have been studied and the results of'the analysis were as follows ;1 . Tlle temperatilre, pH, moisture and organic matter of sampling s'tes were measured in the range of 21.O~28.O$^{\circ}C$, 4.0"6.6, 2.1"24.0% and 2.8~22.0% respectively.and that showed wide range distribution in moisture and organio mattrr particulary.and averase was 24.$^{\circ}C$ of temperature, 4.9 of pH, 11.9% of moisture and 8.9% of'organic matter.2. The general bacterial number, cellulolytic bacterial number, general fungal number and cellulolytic fungal number were measured in tile range of 23$\times$10$^{[-995]}$ _1548x10$^{[-995]}$ , 8.0$\times$10$^{[-995]}$ ~412.0$\times$10$^{[-995]}$ , 0.3$\times$10$^{[-994]}$ ~56.4$\times$10$^{[-994]}$ and 0.Ix10$^{[-994]}$ ~17.2x10$^{[-994]}$ , respectivelyand average was 378.4$\times$10$^{[-995]}$ of general bacteria, 102.5$\times$10$^{[-995]}$ of cellulolytic bacteria.13.OX10$^{[-994]}$ of general fungi and 4.3$\times$10$^{[-994]}$ of cellulolytic fungi.tic fungi.

• 한국지반환경공학회 논문집
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• 제5권1호
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• pp.35-46
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• 2004

화강암질은 우리나라의 3분의 1을 차지하고 있으며, 특히 화강풍화지반은 우리나라 전역에 걸쳐 널리 분포하고 있다. 화강풍화지반은 민감한 입자 구조를 가지고 있어 비교란시료를 채취하기가 매우 어려우며 이로 인해 대부분의 연구는 재성형 시료로 수행되어 지고 있는 실정이다. 그러므로 비교란 또는 재성형 시료로 부터 얻어지는 탄성계수와 감쇠비 등의 변형특성을 비교하는 것은 신뢰성 있는 지반 거동을 이해하는데 중요하다. 본 눈문에서는 국내 화강풍화지반에 대해 다양한 공진주/비틂전단시험을 수행하였다. 그리고 화강풍화지반에 있어 비교란, 재성형 시료 각각의 탄성계수와 감쇠비 등의 변형특성이 비교되고 평가되었다.

• 지질공학
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• 제12권4호
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• pp.459-469
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• 2002

재성형된 해성점토 시료를 연직·수평방향으로 채취하여 표준압밀시험(SCT)과 일정변형률속도 압밀시험(CRSC)을 실시하여 연약 해성점토지반에 대한 압밀정수들의 구성관계를 확인하였다. 또한, 불교란 교란 화강암질 풍화토의 표준·일정변형률속도 압밀시험을 통하여 화강암질 풍화토에 대한 압밀 정수들의 특성과 적용성을 고찰하였다. 그 결과 해성점토 시료의 연직·수평방향과 표준·일정변형률속도압밀시험 방법에 따라 선행압밀응력, 압축지수, 과잉간극수압, 간극수압비 등이 달리 산정됨을 알 수 있었다. 또한, 불교란·교란 화강암질 풍화토 시료에서도 해성점토와 유사하게 과압밑·정규압밀 구간에서 압밀정수들의 변화를 확인하였다.

• 한국환경농학회지
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• 제25권3호
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• pp.262-267
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• 2006

Increased application of glyphosate (Gly) in glyphosate-resistant (GR) soybean cropping systems may affect rhizospheric microorganisms including IAA-producing rhizobacteria (IPR) and their effect on the growth of soybean. This field experiment was conducted to assess IPR populations in the rhizosphere of GR soybean ('Roundup-Ready' DeKalb DKB38-52) treated with glyphosate and foliar amendment treatments such as $PT21^{(R)}$ (urea solution with N 21 %) and $Grozyme^{(R)}$ (Biostimulant: mixtures of micro nutrients and enzymes). Effects of herbicide, sampling date, and their interaction on total bacterial numbers were significant (P < 0.001, 0.001, 0.013, respectively). Total bacteria (TB) numbers were increased with glyphosate treatment at 20 d after application and highest TB populations were associated with $Grozyme^{(R)}$ application, possibly due to the additional substrate from this product. The IPR of the soybean rhizosphere was significantly affected by herbicide, sampling date, and the herbicide*foliar amendment interaction. The ratios of numbers of IPR to TB ranged from 0.79 to 0.99 across the sampling dates irrespective of treatments. IPR numbers were slightly hindered by glyphosate application regardless of foliar amendment.

• 한국토양비료학회지
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• 제46권2호
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• pp.122-128
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• 2013

본 연구는 제주지역 농경지 이용유형과 토양특성별 미생물체량과 탈수소효소활성을 평가 하고자 수행하였다. 제주지역 밭(50), 과수원(50), 논(30), 시설재배(30) 토양을 3월에 채취 후 토양화학성과 탈수소효소활성, 미생물체량을 분석하였다. 밭 토양의 평균 pH는 6.3이었고 과수원, 시설재배지 토양은 조사지점간에 화학성분 함량의 차이가 크게 나타났다. 돈분퇴비를 시용하는 감귤재배농가의 토양 내 아연과 구리함량은 증가하는 경향을 보였다. 토양 탈수소효소활성과 미생물체량은 농경지 이용유형에 상관없이 비화산회 토양이 화산회토양보다 높았다. 탈수소효소활성은 밭 토양이 과수원, 논, 시설재배지 토양보다 2-4배 이상 높았고 비화산회토의 밭토양은 38.7 ug TPF $24^{h-1}g^{-1}$를 나타냈다. 미생물체량은 시설재배지 토양이 가장 많았으며 시설재배지 비화산회토양은 216.8 $mg\;kg^{-1}$였다. 시설재배지의 비화산회토양은 탈수소효소활성과 토양유기물($R^2$=0.59), 아연($R^2$=0.65), 구리($R^2$=0.66)의 함량간에 높은 정의 상관관계를 보였다. 화산회토의 밭토양은 유기물함량과 탈수소효소 활성간에 높은 부의상관관계($R^2$=0.57)를 나타냈다.

• 한국토양비료학회지
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• 제45권2호
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• pp.312-316
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• 2012

1. 우리나라 북부 8개 지역을 대상으로 하여 최근 30년간의 기상자료 분석에 의한 12월~6월의 일평균 PET는 $2.31mm\;day^{-1}$ 이었다. 2. 시설재배 고추의 우리나라 북부 8개 지역별, 3개 토성 및 16개 순별, 총 384경우의 재배여건에 적합한 물 절약형 적정 관개간격 및 1회 관개량을 산정하였다.

• 한국토양비료학회지
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• 제49권5호
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• pp.524-530
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• 2016

Agricultural soils near or around industrial complexes can contain a certain amount of heavy metals that readily enter the food chain and negatively affect human health. Therefore, we conducted the study to investigate the distribution of selected heavy metals, including arsenic (As), cadmium (Cd), chromium (Cr), nickel (Ni), lead (Pb), mercury (Hg), and zinc (Zn), in farm-land soils around fifteen industrial complexes in the southwestern provinces, Korea. The concentrations of heavy metals in the soil samples were determined by the pseudo-total aqua regia (3 HCl : $1HNO_3$) digestion procedure. The heavy metal concentrations in most soils examined did not exceed the levels of Soil Contamination Warning Standard (SCWS) for agricultural lands (Region 1) presented in Soil Environment Conservation Law (SECL) established by Ministry of Environment (MOE), Korea. However, only one sampling site showed higher As amount ($27.1mg\;kg^{-1}$) than the SCWS level of As ($25mg\;kg^{-1}$). Pollution index (PI) for heavy metals did not exceed 1.0. The PI values were significantly positively correlated (p < 0.01) with the heavy metal concentrations. In particular, the values of correlation coefficient between the Cd and Pb concentrations and the PI values were higher than those estimated from other combinations, and thus the amounts of Cd and Pb in the agricultural soils highly affected the PI values for the heavy metals.

• 한국환경과학회지
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• 제12권2호
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• pp.93-100
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• 2003

In most mountainous parts of the temperate zone of Japan along the Pacific Ocean, some climatic climax forests, whose main dominant species is Fagus crenate, F. japonica or Quercus mongolica var. grosseserrata, are distributed. In the riparian regions of the zone, however, there appear summer green forests composed of the different species from the climatic climax forests. Climate plays an important role in determining the overall distribution of vegetation, but some environmental factors, i.e., topography, soil type, soil moisture content, etc. have a great influence on vegetation formation. Riparian forests seem to be controlled by various geomorphologic disturbances, such as landslide, soil erosion and accumulation. The study aims to present the relationships among vegetation, soils and landforms in the process of determining riparian forests dominated by Fraxinus platypoda and Pterocarya rhoifolia establishment in the mountainous region of central Japan. The study area extends an area of 302 ha with a range of elevation between 925 m and 1,681 m at the Chichibu mountains. The landforms were corditied at sampling grids (25 $\times$ 25 m, n = 4,843) using a hierarchical system, and a brief description of the forest soil classification was also given. The mutual relationship analysis indicated that forest soils and landforms play a significant role in determining the geomorphological process of riparian forest, and shaping the ultimate pattern of vegetation. At the study area, riparian forests were mainly found on the $B_E$ forest soil type and steep slopes ( > 30$^{\circ}$) at convex slopes along the streams. On the other hand, the direction of slopes did not have a significant impact on the establishment of the riparian forests. A mosaic of patchy distribution of those riparian forests on the slightly wetter $B_E$ forest soil type was one of the characteristic features of the study area. This particular soil which contained large talus gravels was found on the land formed by erosion and deposition of landslide.