• Korean Journal of Environment and Ecology
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• v.13 no.2
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• pp.176-183
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• 1999

울산지역의 사문암과 유문암 토양 및 쑥과 참억새의 중금속 함량을 비교하기 위하여 중금속 농도를 분석한 결과 사문암 풍화토의 Ni, Cr 및 Co 함량은 매우 높았다. Ni은 1,483~1.524ppm, Cr은 372~435ppm, Co는 68~79ppm였으며, 유문암 풍화토의 Zn 함량은 222ppm으로 사문암 풍화토보다 높았다. 사문암 풍화토에서 생육하는 쑥의 중금속 함량은 Ni이 108~195ppm. Cr이 135~180ppm, Co가 10.2~22.5ppm으로 유문암 풍화토의 쑥보다 높았고, Zn은 유문암 토양 쑥에서 높았다. 참억새의 경우는 Ni, Cr, Co, As, Se, Mo 및 Fe 가 사문암 토양에서 높았고, Zn 흡수는 유문암 토양에서 많았다. 쑥의 중금속 함량은 대체적으로 지상부가 지하부보다 높았으나, 참억새의 경우는 지하부가 높은 경향을 나타내었다. 토양과 식물체(쑥과 참억새)의 중금속 함량을 비교해 보면 Ni, Cr, Co, As, Sc, Mo 및 Fe의 함량은 토양의 식물체보다 높았으나, 유문암 토양에 있는 쑥의 Zn 흡수는 토양보다 다소 높았다. 식물체의 Fe:Ni 비율은 유문암 토양보다는 사문암 토양이, 참억새보다는 쑥이 낮게 나타났다.

• Proceedings of the International Microelectronics And Packaging Society Conference
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• 2003.11a
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• pp.88-93
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• 2003

무전해 Ni-P와 Sn의 반응 및 Ni-P의 결정화에 대한 P 함량의 영향을 세 가지 다른 조성의 Ni-P (P 4.6, 9, 13 $wt.\%$)를 이용하여 연구하였다. $300^{\circ}C$까지 열처리한 모든 시편에서 $Ni_3Sn_4$ intermetallic compound (IMC)가 생성되었고 이들 시편을 $450^{\circ}C$까지 열처리한 경우 Sn 두께가 $0.5{\mu}m$로 작을 때 $Ni_3Sn_4$가 모두 $Ni_3Sn_2$로 변화하였다. nanocrystal인 Ni-4.6P는 Ni (111) texture를 유지하며 결정화되었고 Sn과의 반응시 형성되는 $Ni_3Sn_4$ IMC 또한 비정질인 Ni-9P, Ni-13P 경우보다 강한 (111) texture를 가짐이 확인되었다. Ni-P 막의 P 함량이 작은 경우 $Ni_3Sn_4$ IMC는 두껍고 조밀하게 형성되는 반면 P-rich layer 두께는 작아졌다.

• Analytical Science and Technology
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• v.12 no.1
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• pp.40-46
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• 1999

Zn-Ni alloy electrodeposition on steel has been examined by means of X-ray diffraction and scanning electron microscopy. The effect of current density, $Ni^{2+}$ ion concentration, and $Cl^-$ ion concentration on the structure as well as morphology of the electrodeposit have been studied. The Ni content of the electrodeposit increased with decreasing current density in the range studied in this work. The Ni content of the electrodeposit also increased with increasing $Ni^{2+}$ ion and $Cl^-$ ion concentrations. The structure change of the electrodeposit was closely related to the Ni content. In fact, the mixture phase of ${\eta}$ and ${\gamma}$ was found below 10 wt.% of Ni while the ${\gamma}$ phase only was observed above 10 wt.% of Ni. In addition, the lattice parameter, a, of then phase structure increased and the lattice parameter, c, of it decreased as the Ni content of the electrodeposit increased. The morphology of the electrodeposit varied from the plate-like shape to the fine granular shape depending upon the change in composition and structure of the electrodeposit.

• Korean Journal of Environment and Ecology
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• v.12 no.1
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• pp.22-29
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• 1998

This study is investigated for the trace element concentration in the soils derived from different parent rocks, which are serpentinites, metamorphic rocks and black shales, and the absorption of the trace element by Pinus rigida in Hongseong and Keumsan, Chungnam, respectively. The concentrations of nickel, chrominium and cobalt are high in the serpentinites, whereas the concentrations of zinc, molybdenium and iron are high in the metamorphic rocks. These elements in black shale are lower than those in serpentinites and metamorphic rocks. The serpentine soils show high nickel, chrominium and cobalt content, while zinc and iron content are high in the mixed soils(serpentinites + metamorphic rocks) and black shales. Comparing with parent rocks, all of trace elements in their weathered soils are low. The pH of serpentine soil is high, 7.73~9.55 and that of black shale soil in 5.61. In serpentine area, the absorptions of chrominium by P. rigida is lower than its in the soils. The absorption of zinc by P. rigida is high relative to zinc concentration in soils. The Co/Ni and Fe/Ni quotient in P. rigida over serpentine soils are considerably lower than those growing over other soils tpes.

• Korean Journal of Soil Science and Fertilizer
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• v.41 no.3
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• pp.199-205
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• 2008

This study was carried out to find out causes of high Ni content and characteristics of potential increase of Cu and Zn contents in the soils of Jeju area. Soil samples were collected from 4 series of Alfisols, 35 series of Andisols, 9 series of Entisols, 16 series of Inceptisols, and 1 series of Ultisols, respectively. Parent material (gravel) samples were also collected from the same sites where soil samples were taken. Both soil and parent material samples were analyzed for Ni, Cu, and Zn. The average Ni content of all the soil samples was $79.2mg\;kg^{-1}$, which was exceeded warning standard for Ni against the Soil Conservation Act in Korea, whereas that of Cu and Zn contents were lower than the warning standard for Cu and Zn. The difference of Ni, Cu and Zn content was not consistent depending upon soil color. Ni content in the soil samples from Entisols was particularly high, whereas that from the other soil orders was similar to each other. Cu and Zn contents in the soil samples were similar regardless of the difference in soil order. Ni content in Seongsan Formation(SSF), Cinder cone(C) and acicular Feldspar Olivine Basalt(FOB) was high, while that in Feldspar Basalt(FB) and Trachy Andesite lava(TA) was low. Ni content in the non-agricultural land was higher compared with that in the agricultural land, whereas Cu and Zn contents in the non-agricultural land were significantly lower than that of agricultural land. The topsoil/subsoil ratios for Ni content in most of the soil samples were less than 1, while that for total contents of Cu and Zn in many of the soil samples were larger than 1 indicating potential Cu and Zn accumulation in topsoil by artificial reasons.

• Proceedings of the Korean Institute of Surface Engineering Conference
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• 2015.11a
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• pp.151-153
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• 2015

무전해도금법을 이용하여 Ag/Ni 코팅 Cu 플레이크를 제조한 후 Ni 코팅층의 P 함량에 따른 Ag dewtting 거동에 대한 연구를 수행하였다. Ni 코팅층 내 P 함량이 낮을수록 Ni 코팅층의 결정성 및 결정화 속도가 높아지는 것을 알 수 있었으며, 이는 Ni 코팅층 위에 형성된 Ag 코팅층의 dewetting 거동에 영향을 주는 것으로 분석되었다. 또한 격자 불일치도가 높을수록 잘 발생하는 dewetting 현상은 P 함량이 높아 결정성이 떨어지는 Ni 코팅층에서 더욱 빨리 일어남을 알 수 있었다.

• Proceedings of the Materials Research Society of Korea Conference
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• 2009.11a
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• pp.46.2-46.2
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• 2009

휴대전화, 랩톱 컴퓨터 등 각종 모바일기기 및 디스플레이 기기의 경박단소화 및 고기능화에 따라 연성회로기판(FPCB)의 사용량이 증가하고있다. 연성회로기판의 핵심소재인 동박적층필름(FCCL)은 폴리이미드필름과 접착층, Cu 층으로 구성되는데, 이 중접착층으로 사용되는 Ni-20Cr합금은 에칭공정 후 Cr의 잔류에 의해 불량률 증가가 문제되고 있어, Ni-Cr합금 스퍼터링 타깃의 Cr 함량 저감 또는 Cr-free Ni합금 개발 등이 요구되고 있다. 본 연구에서는 차세대 FCCL 본드층에 적합한 Ni기 합금을 개발하기 위한 기초연구로써 Cr 함량 및 가공열처리조건에 따른 미세조직과 집합조직 변화를 조사하였다. 4N급의 고순도Ni과 Cr을 진공 플라즈마 용해장치로 용해하여Ni-xCr (x=5, 10, 15, 20wt.%)합금 잉곳을 만들고, 이를 두께감소율 90%로 냉간압연한 후, $600^{\circ}C$ 및 $800^{\circ}C$에서 10~120분 동안 어닐링하여 시편을 준비하였다. 광학현미경으로 미세조직을 관찰하고, Micro-Vickers 경도시험을 통해 어닐링 조건에 따른 경도변화를 조사하였다. 또한 SEM-EBSD를 이용하여 집합조직 및 입계특성을 분석하였다. $600^{\circ}C$ 어닐링 시 Cr함량이 증가할수록 재결정 완료시간이 증가하여 Ni-20Cr합금의 경우 2시간이상 어닐링에도 재결정이 일어나지 않았다. $800^{\circ}C$ 어닐링 시 10분 어닐링 조건에서 4종류 합금 모두 재결정이 완료되었으며, 동일한 어닐링 조건에서 Cr함량이 증가할수록 결정립이 작아지는 것으로 나타났다. $800^{\circ}C$ 2시간 어닐링 조건에서 Ni-5Cr 합금의 주요 집합조직은 {223}<113>과 {122}<112>로 나타났으며, 이중 {223}<113>은Cr 함량이 증가함에 따라 점차 {122}<112>에 가까운 방향으로 변화되어 Ni-20Cr 합금의 경우 {123}<112>만이 형성되었다. 이러한 집합조직의 변화는 적층결함에너지 감소에 의한 ${\Sigma}3$ 입계의 분율 증가와 밀접한 관련이 있는 것으로 사료된다.

• Journal of Korea Foundry Society
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• v.23 no.3
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• pp.147-152
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• 2003

질소 용해도가 낮은 ${\delta}$상으로 응고가 시작되는 16Cr-3Ni 계 스테인리스강의 응고시 질소기포 형성에 미치는 질소 함량과 냉각속도의 영향이 조사되었으며 이를 기반으로 질소 기포 결함이 발생하는 임계 질소 함량을 예측하는 방법을 제시하였다. 질소함량의 증가는 질소 기포 결함을 증가시켰으며, 냉각속도의 증가는 질소기포결함의 형성을 다소 억제 할 수 있는 것으로 조사되었다. 실험적으로 구한 Fe-16Cr-3Ni-9Mn 합금의 임계 질소 함량은 0.19wt%였으며, 임계 질소 압력은 평형응고로 가정한 경우 1.27atm, Scheil 응고로 가정한 경우에는 1.23atm으로 계산되었다. 질소 용해도를 증가시킬 수 있는 Mn 함량의 변화에 따른 임계 질소 함량의 변화를 예측하기 위하여 계산된 임계 질소 압력을 Fe-16Cr-3Ni-11Mn 합금에 적용하였으며 이를 통해 얻은 임계 질소 함량은 평형응고로 가정한 경우 0.25wt%, Scheil 응고로 가정한 경우에는 0.24wt% 로 예측되었다. 예측 결과의 타당성을 확인하기 위하여 Fe-16Cr-3Ni-11Mn 합금의 실험 결과와 비교하였으며, 일치하는 결과가 얻어졌다.

• Korean Journal of Soil Science and Fertilizer
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• v.40 no.2
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• pp.164-171
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• 2007

This experiment was conducted to investigate heavy metal speciation and bioavailability from soil to the edible parts of water dropwort near industrial complex. The soils and water dropwort were collected from the paddies cultivating water dropwort(10 sites), stream sediments(5 sites), and background soils(3 sites) near industrial complex. The total concentrations of Cd Cu, and Ni were higher than those of permissible level for soil contamination(Cd 3, Cu 100, Ni $50mg\;kg^{-1}$ in soil) suggested by Kloke(1979). Dominant chemical forms of Cd in paddies cultivating water dropwort and stream sediments were exchangeable form(49.1-56.3%), and those of Cu, Zn, and Ni were Fe and Mn oxide bound and residual forms. The mobility factor of heavy metals in paddies cultivating water dropwort and stream sediments was in the order Cd>Zn>Ni>Cu>Pb, specially, the mobility factor of Cd (62-72%) were relatively higher than that of other metals in soils. The total concentrations of Cd in soils showed significant positive correlation with the ratios of exchangeable and Fe and Mn oxide bound forms, while correlated negatively with residual form. Heavy metal contents in root parts were higher than those in top parts of water dropwort. The bioavailability of water dropwort varied considerably between the different parts and heavy metals. Cd, Cu and Ni contents in water dropwort were correlated with each fractions in soils. Specially, the exchangeable form of Cd and Ni in soils showed significant positive correlation with the those contents of water dropwort.

• Journal of Korea Soil Environment Society
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• v.4 no.2
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• pp.113-125
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• 1999

Heavy metal elements were analysed to assess degrees of heavy metal contents for the plants, M. sinensis, A. vulgaris and G. oldhamiana, from the Baekdong serpentine area within the western part of Chungnam. The area was divided into two sites ; serpentine area (SP, consisting of serpentinite, SP) and non-serpentine area (NSP, containing amphibole schist, AS and gneiss, GN). Their host rocks(R) and top soils(S) were also collected from the each site. As the results of the study, the plants contain high concentration of Ni Cr, Co in the SP and Fe, Zn in the AS and GN. Plants from the AS of the NSP contain mainly high content in the most of elements. Averages of Ni, Co and Cr for the plants decreased in the order of SP, AS and GN. In the total element contents, M. sinensis and A. vulgaris decreased in the order of Fe > Ni or Cr > Zn > Co > As > Sc within the SP and in the order of Fe > Zn > Cr > Ni, within the GN. Comparing among the parts of plants, root parts were higher in the most of elements than the above grounds. In the relative element ratios of plants collected from the SP and GN (SP/GN) M. sinensis was lower than A. vulgaris in the most of elements, suggesting that the M. sinenis shows low absorption within the infertile serpentine soil and high absorption within the fertile gneiss soil. In the element contents of the top soils and their host rocks, the SP shows higher Ni, Co and Cr contents than the others. Their total contents decreased from SP to AS and GN, suggesting that the soils reflect the composition of their host rocks. Total element contents of the SP decreased in the order of Fe> Cr or Ni> Co> Zn> As> Sc and, for the GN, in the order of Fe> Zn> Cr> Ni> Co or Sc, respectively. In the relative element ratios, R/S of the SP decreased in the order of Cr> As> Fe> Sc> Co> Ni> Zn and for the GN, in the order of Sc> Fe> Ni> Zn> Cr> Co. Comparing with plants within the each site, their top soils were higher than the plants in the most of elements. and their increase and decrease trends for each element are similar. Differences of element contents between the top soils and plants decreased in the order of SP, AS and GN. Plants of the GN were moi-e similar to their soils than those of the others, suggesting that each plant species show different absorptions within the different soils. Comparing with the plants of GN, higher Ni, Co, Cr contents within those of the SP and their survival within the infertile serpentine soil suggest that the M. sinensis, A vulgaris and G. oldhamiana may be the tolerance species in the serpentine soil. Comparisons with the upper crust show that M. sinensis, and A. vulgaris within the SP show high Hi and Cr contents. suggestive of hyperaccumulation. Upper results with the previous studies for the contaminated soils developed as parent materials with the serpentinites suggest additional studies for ecological behaviors for the plant and degrees of accumulations for the elements need to know phytoextraction of the heavy metal elements within the soils.