• 한국수소및신에너지학회논문집
• /
• 제19권4호
• /
• pp.340-347
• /
• 2008

Dissolution process of serpentine in distilled water was systematically investigated for study on pre-treatment of serpentine which was a candidate material for carbon dioxide sequestration. The metallic ions(Ca, Si, Mg etc.) were dissolved in distilled water at ambient condition and their concentrations were changed with dissolution time. The precise evaluation of dissolution process for serpentine dissolved solvent was performed by ion conductivity and pH measurement. Serpentine dissolution in distilled water was evaluated as a stable pre-treatment process without changes of crystallographic structure and chemical structure changes.

• 한국광물학회지
• /
• 제9권2호
• /
• pp.102-112
• /
• 1996

The precious serpentine, referring to a rare and highly valuable gem variety of serpentine group minerals, is found to occur in serpentinite from Booyo Gren Jade Mine which is located in Oesan-myun, Booyo-gun of Chungchungnam-do. Geommological properties of the precious serpentine have been investigated by use of polarizing microscope, specific gravity balance, refractometer, hardness pencils, X-ray diffractometer, XRF, ICP-MS analyser, and infrared absorption spectroscope.The precious serpentine from Booyo is colored deep green with oily luster and semi-transparent. It is highly tough and Mohs's scale of hardness is measured to be 5-6. Specific gravity is determined to be 2.67, and a single refractive index ND=1.56 is observed by a spot method, using sodium light source. X-ray powder diffraction data is represented by the reflection lines at 7.40(100), 4.64(25), 3.68(68), 2.757(69), 2.530(49), 2.549(32), and 1.710(21${\AA}$), which compares very well with that of antigorite of serpentine group minerals. The major chemical compositions of the precious serpentine group minerals. The major chemical compositions of the precious serpentine are SiO2 42.49%, MgO 39.08%, Fe2O3 3.85%, and H2O 11.87%. Besides, trace elements such as Cr(2188), Ni(1110ppm), Co(58ppm), and Ta (108ppm) are relatively spectrum shows peaks at 3670, 1190, 1070, 980 and 610cm-1. Strong absorption at 3670cm-1 is due to OH stretching, and 1190, 1070 and 980cm-1 due to SiO stretching. The absorption 610cm-1 is formed by alteration of pre-existing ultramafic rock, namely peridotite, with an introduction of fluid with very little content of CO2, under 400$^{\circ}C$ environment. Magnetite inclusions, finely disseminated in the precious serpentine, may be a result of Fe precipitation, during serpentinization of olivine-bearing country rock.

• 한국산업보건학회지
• /
• 제23권1호
• /
• pp.35-40
• /
• 2013

Objectives: Asbestos contents of crushed serpentine rocks and airborne fiber concentrations of workers were determined at two serpentine quarries and a steel mill. Methods: Bulk samples of uncrushed and crushed serpentine rocks were collected and analyzed by PLM and TEM. Airborne asbestos samples were collected from the breathing zone of workers and the vicinity of working area and analyzed by PCM and TEM. Results: Chrysotile was identified with antigorite, lizardite and non-asbestiform actinolite in bulk samples. The arithmetic means of chrysotile contents in crushed serpentines were 0.11, 0.01, 0.42%(W/W) by quarry A, quarry B and a steel mill, respectively. The asbestos concentrations of all personal samples were less than 0.1 f/cc which is the permissible exposure limit of workers in Korea. The arithmetic means of airborne asbestos concentrations were 0.017 f/cc and 0.009 f/cc in personal samples collected from two serpentine quarries. The asbestos concentrations of all personal samples collected from a steel mill were less than LODs by PCM analysis but asbestos was detected in area samples by TEM. By the job tasks of serpentine quarries, crusher/separator operation generated the highest exposure to airborne asbestos. Conclusions: Although chrysotile contents in crushed serpentines of quarries were less the permissible level, the highest exposure of workers in serpentine quarries reached up to 76% of the permissible level of airborne asbestos. There were also possibilities of occupational exposure to airborne asbestos in a steel mill. The present exposure study should encourage further survey and occupational control of quarries producing serpentine or other types of asbestos-bearing rocks.

• 공업화학
• /
• 제21권1호
• /
• pp.24-28
• /
• 2010

이산화탄소의 광물고정화는 자연계의 풍화 작용을 모사한 것으로 매우 안정한 반응이지만 반응 속도가 매우 느리다. 이러한 반응 속도 증가를 위하여 광물의 전처리가 필요하다. 본 연구에서는 이산화탄소 광물고정화 속도 증가를 위한 두 가지의 전처리 방법을 소개하고 고정화 효율 증가를 확인하였다. 열적전처리는 $630^{\circ}C$에서 행해지는데, 이는 이산화탄소가 고정화되는 것을 방해하는 사문석 분자 내의 -OH기의 제거한다. FT-IR 피크를 통해 -OH기가 제거되는 것을 확인할 수 있다. 화학적전처리는 사문석 내의 주요 광물고정화 성분인 마그네슘 성분을 $75^{\circ}C$의 추출 온도에서 황산을 이용하여 추출해내는 것이다. 황산의 수소이온이 사문석 내의 결합을 약화시켜 마그네슘이 추출되도록 한다. 이는 ICP-AES와 XRF를 통하여 추출량을 확인하였다. 전처리가 끝난 사문석을 이용하여 이산화탄소 광물고정화 반응을 진행시 열적전처리의 경우 43%의 이산화탄소 고정화 효율을 나타내는데, 전처리를 하지 않았을 때 27%의 효율에 비하여 증가하였음을 확인하였다. 하지만 이 경우 많은 에너지가 소비된다는 단점이 있다. 화학적 전처리의 경우 열적전처리에 비해 45 atm, $25^{\circ}C$라는 비교적 온화한 조건에서 진행되는데, 이산화탄소 고정화 효율도 전처리 전인 24%에서 42%까지 상승하는 것을 확인할 수 있다.

• 한국환경생태학회지
• /
• 제32권6호
• /
• pp.676-685
• /
• 2018

경북 안동 사문암 지역의 소나무군락에서 2017년 01월부터 2017년 12월까지 1년간 매목조사, 미기상 및 토양호흡 측정을 통해 탄소수지를 측정하였다. 사문암 지역에서 토양호흡량은 연중 42.48 ~ 262.61 g $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$의 범위로, 평균 $151.71{\pm}75.09g$ $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$로 측정되었다. 대조구인 비사문암 지역의 소나무림에서는 연중 20.94 ~ 449.24 g $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$의 범위로 조사되었으며, 평균 $165.09{\pm}118.96g$ $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$로 측정되었다. 사문암 지역과 비사문암 지역의 총 탄소저장량은 각각 91.90, $222.85ton{\cdot}ha^{-1}$로 나타났으며, 연간 탄소흡수량은 각각 7.99, $17.41ton{\cdot}ha^{-1}{\cdot}yr^{-1}$로 나타났다. 사문암 지역은 연간 $5.3tonC{\cdot}ha^{-1}$, 비사문암 지역은 연간 $14.49tonC{\cdot}ha^{-1}$를 흡수하는 것으로 나타났다.

• 한국광물학회지
• /
• 제25권1호
• /
• pp.9-21
• /
• 2012

우리나라에는 약 6개소의 사문석광산이 존재하였으며, 그 중에 최근까지 채굴되었던 충남지역의 비봉광산에 대하여 구성광물의 산출상태, 특성 및 성인을 검토하였다. X-선회절분석, X-선형광분석, 주사현미분석, 전자현미분석, 적외선분광분석, 편광현미경관찰 등을 통하여 사문석의 광물학적 특성을 조사하였다. 비봉광산의 사문암체는 선캠브리아기의 변성퇴적암을 관입한 형태로 소규모로 분포하여 나타나며, 사문석, 포스터라이트, 휘석, 투각섬석, 자철석, 녹니석, 운모, 활석, 돌로마이트 등의 다양한 광물들이 산출되었다. 사문암체의 광물조합은 크게 A) 사문석-포스터라이트, B) 사문석, C) 사문석-녹니석(버미큘라이트), D) 사문석-투각섬석, E) 투각섬석-녹니석의 5가지로 구분되어 나타났다. 사문석광물은 리자르다이트와 안티고라이트가 주로 포함되며 크리소타일은 일부 부분적으로 포함되어 산출되는 것으로 나타났다. 사문암체의 구성광물과 그 산출상태로 보아 포스터라이트를 주성분으로 하는 초염기성암의 열수변질작용에 의해 사문석이 형성되었으며, 그후 2차적인 열수작용에 의해 녹니석과 투각섬석 등의 변질광물이 형성된 것으로 나타났다.

• 한국정밀공학회:학술대회논문집
• /
• 한국정밀공학회 2004년도 추계학술대회 논문집
• /
• pp.756-759
• /
• 2004

We present a piezoelectric actuator using stiffness control and stroke amplification mechanism in order to make large lateral displacement. In this work, we suggest stiffness control approach that generates lateral displacement by increasing the vertical stiffness and reducing the lateral stiffness using additional structure. In addition, an additional structure of a serpentine spring amplifies the lateral displacement like leverage structure. The suggested lateral PZT actuator (bellows actuator) consists of serpentine spring and PZT/electrode layer which is located at the edge of the serpentine spring. The edge of the serpentine spring prevents the vertical motion of PZT layer, while the other edge of the serpentine spring makes stroke amplification like leverage structure. We have determined dimensions of the bellows actuator using ANSYS simulation. Length, width and thickness of PZT layer are 135$\mu$m, 20$\mu$m and 0.4$\mu$m, respectively. Dimensions of the silicon serpentine spring are thickness of 25$\mu$m, length of 300$\mu$m, and width of 5$\mu$m. The bellows actuator has been fabricated by SOI wafer with 25$\mu$m-top silicon and 1$\mu$m-buried oxide layer. The bellows actuator shows the maximum 3.93$\pm$0.2$\mu$m lateral displacement at 16V with 1Hz sinusoidal voltage input. In the frequency response test, the fabricated bellows actuator showed consistent displacement from 1Hz to 1kHz at 10V. From experimental study, we found the bellows actuator using thin film PZT and silicon serpentine spring generated mainly laterally displacement not vertical displacement at 16V, and serpentine spring played role of stroke amplification.

• Advances in nano research
• /
• 제12권2호
• /
• pp.151-165
• /
• 2022

Micro-scale serpentine structure fibers are widely used as flexible sensor in the manufacturing of micro-nano flexible electronic devices because of their outstanding non-linear mechanical properties and organizational flexibility. The use of melt electrowriting (MEW) technology, combined with the axial bending effect of the Taylor cone jet in the process, can achieve the micro-scale serpentine structure fibers. Due to the interference of the process parameters, it is still challenging to achieve the precise deposition of micro-scale and high-consistency serpentine structure fibers. In this paper, the micro-scale serpentine structure fiber is produced by MEW combined with axial bending effect. Based on the controlled deposition of MEW, applied voltage, collector speed, nozzle height and nozzle diameter are adjusted to achieve the precise deposition of micro-scale serpentine structure fibers with different morphologies in a single motion dimension. Finally, the influence mechanism of the above four parameters on the precise deposition of micro-scale serpentine fibers is explored.

• The Korean Journal of Ecology
• /
• 제20권5호
• /
• pp.385-391
• /
• 1997

충남 광천과 홍성 일대의 사문암과 변성암 지역의 암석, 토양 및 출현빈도가 높은 대나물의 중금속 함량을 측정하여 사문암 토양의 독성화 정도와 식물체의 흡수관계를 조사하였다. Ni, Cr 및 Co는 사문암에 매우 높았으며 Zn, Sc, Mo 및 Fe 는 변성암에서 더 높았다. 사문암 풍화토에서는 Ni, Cr 및 Co가 높았으며 Zn과 Fe는 비사문암 풍화토(사문암 및 변성암 풍화토와 변성암 풍화토)에서 높았고, 토양의 중금속은 암석내의 함량보다 낮았다. 사문암 풍화토에 출현하는 대나물내 중금속 함량은 혼합 풍화토의 그것보다 높게 나타났으며, 같은 사문암 지역이라도 홍성보다 광천의 중금속 함량이 높았다. 대나물의 평균 Fe:Ni의 비율은 혼합 풍화토에서는 216이고 사문암 풍화토에서는 49였다. 대나물내 Ni, Cr, Co, Fe 및 Sc 등은 지상부보다 지하부에서 높았으며, Zn과 Mo 함량은 지상부에서 높았다. 암석과 식물체의 중금속 함량 비교 결과 식물체에서보다 암석의 중금속 함량이 높았고, 대나물에 의한 Zn의 흡수는 사문암과 변성암 지역에서 높았으며 Sc와 Fe는 사문암 지역에서 뚜렷이 높았다.

• 대한기계학회논문집B
• /
• 제33권4호
• /
• pp.288-297
• /
• 2009

A serpentine channel geometry often used in a fuel cell has a strong pressure gradient between adjacent channels in specific regions. The pressure gradient helps some amount of reactant gas penetrate through a gas diffusion layer(GDL). As a result, the overall serpentine flow structure is slightly different from the intention of a designer. The purpose of this paper is to examine the effect of serpentine flow structure on current density distribution. By using a commercial code, STAR-CD, a numerical simulation is performed to analyze the fuel cell with high aspect ratio of active area. To increase the accuracy of the numerical simulation, GDL permeabilities are measured with various compressive forces. Three-dimensional flow field and current density distribution are calculated. For the verification of the numerical simulation results, water condensation process in the cathode channel is observed through a transparent bipolar plate. The result of this study shows that the region of relatively low current density corresponds that of dropwise condensation in cathode channels.