• 제목/요약/키워드: $SiO_2-Al_2O_3$

검색결과 2,252건 처리시간 0.025초

포항-울산간의 점토자원의 지질과 그 물리화학적 특성에 관한 연구 (A Study on Geology of Clay Mineral Deposits of Pohang-Ulsan Area and their Physico-Chemical Properties)

  • 김옥준;이하영;김서운;김수진
    • 자원환경지질
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    • 제4권4호
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    • pp.167-215
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    • 1971
  • I. Purpose and Importance of the Study The purpose of the present study is to clarify to geological, mineralogical, and physico-chemical properties of the clay minerals deposits imbedded in the Tertiary sediments in the areas between. Pohang and Ulsan along southeastern coastal region of Korea. These clays are being mined and utilized for filter and insecticide after activation or simple pulverizing, nontheless activated clays are short coming as chemical industry in Korea has been rapidly grown in recent years. In spite of such increase in clay demand, no goological investigation on clay deposits nor physico-chemical properties of the clays have been carried out up to date. Consequently activated clays produced in Korea is not only of low grade but also of shortage in supply, so that Korea has to import activated clays of better grade. The importance of the present study lies, therefore, on that guiding principle could be laid down by knowing stratigraphical horizons, of clay deposits and fundamental data of improving grade of activated clays might be derived from the results of physico-chemical examinations. II. Contents and Scope of the study The contents of the study are pinpointed down in the following two subjects: 1) General geological investigation of Tertiary formations distributed in the areas between Pohang and UIsan, and detail geological study of the bentonitic clay deposits imbedded in them. 2) To clarifty physico-chemical characteristics of the clays by means of chemical analysis, X-ray diffraction and electron microscope. The scope of the study involves the following there points: i) Regional geological investigation-This investigation has been carried out in order to find out the distribution of Tertiary sediments and exact location of clay mineral deposits in the areas between Pohang and UIsan. ii) Detail geological investigation-This has been concentrated in and around the clay deposits which. had been found out by the regional investigation. iii) Laboratory researchs include i) age determination and correlation of Tertiary sediments by paleontological study, and ii) Chemical analysis, X-ray diffraction, and electron microscopic studies on clays, samples taken from various clay deposits. III. Research Results and Suggestions 1) The geology of the area investigated is composed mainly of Janggi and Beomgokri groups of Miocene age in ascending order rested on the upper Silla system, Balkuksa granite and volcanic rocks of upper Cretaceous age as base. 2) Janggi group is composed in ascending order of Janggi conglomerate, Nultaeri rhyolitic tuff, Keumkwangdong shale, two beds of lignite-bearing formations which consist of alternation of conglomerate, sandstone and mudstone, and andesitic, rhyolitic, and basaltic tuff beds. 3) Beomgokri group is mainly composed of andesitic to rhyolitic tuff interlayered by conglomerate and tuffaceous sandstone. In the areas around boundary between North-and South Kyeongsang-do is distributed Haseori farmation which is composed of conglomerate, sandstone, mudstone and andesitic to rhyolitic tuff, and which is correlated to Eoilri formation of Janggi group. 4) Clay deposits of the area are interbedded in Eoilri, Haseori, Nultaeri tuff, Keumkwangdong shale, upper and lower horizon of the lower lignite-bearing seam, and Keumori rhyolitic tuff formations of Janggi group; and are genetically classi.fied into four categories, that is, i) those derived from volcanic ash beds(Haseori and Daeanri deposits), ii) those of secondary residual type from rhyolitic tuff beds(Seokupri deposits), iii) Clay beds above and beneath the lignite seams, (Janggi and Keumkwangdong deposits), and iv) those derived from rhyolitic tuff beds(Sangjeong and Tonghae deposits). 5) Mineral constituents of clay deposits are, according to X-ray diffraction, montmorillonite accompanied in different degree by cristobalite, plagioclase, quartz, stilbite, and halloysite in rare occasion. The clays are grouped according to mineral composition into four types; i) those consist mostly of montmorillonite, ii) those composed of montmorillonite and cristobalite, iii) those composed of montmorillonite and plagioclase, and iv) those composed of montmorillonite, plagioclase and quartz. 6) Clays interbedded in Haseori formation and vicinity of lignite seams belong to the first type, are of good quality and derived either from volcanic ash bed, or primary clay beds near lignite seams. Clays belonged to other types are derived from weathering of rhyolitic tuff formations and their quality varies depending upon original composition and degree of weathering. Few clays in secondary residual type contain small amount of halloysite. 7) Judging from analytical data, content of silica($SiO_2$) varies proportionally with content of cristobalite, and alumina($Al_2O_3$) content does not vary with that of plagioclase, but increases in the sedimentary bedded type of deposits. 8) It is unknown whether or not these days could be upgraded by beneficiation since no grain size of these impurities nor beneficiation test had been studied. 9) Clay beds derived from valcanic ash layers or sedimentary layers at the vicinity of lignite seams are thin in thickness and of small, discontinueous lenticular shape, although they are of good quality; and those derived from rhyolitic tuff formations or residual type from tuff are irregular in both occurrence and quality. It is, therefore, not only very difficult but also meaningless to calculate its reserve, and reserve estimation, even if done, will greatly be deviated from practically minable one. Consequently, way of discovery and exploitation of clay deposits in the area under consideration is to check the geologically favorable areas whenever needed.

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Flip Chip의 Solder Bump 형성을 위한 Ni/Au 무전해 도금 공정 연구 (Ni/Au Electroless Plating for Solder Bump Formation in Flip Chip)

  • 조민교;오무형;이원해;박종완
    • 한국재료학회지
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    • 제6권7호
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    • pp.700-708
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    • 1996
  • Flip chip bonding에 무전해도금기술을 적용하여 solder bumper형성의 최적 조건을 규명하였다. 시편은 AI 패턴된 4 inch Si 웨이퍼를 사용하고, 활성화 처리시 zincate 용액을 사용하였으며, 무전해 도금은 Ni-P 도금액고 Au immersion 용액을 사용하였다. 활성화 물질의 AI 침식정도 및 Zn 석출 정도를 알아보기 위하여 EDS측정을 하였고, 각 공전에서의 표면형상을 알아보기 위해 SEM 분석을 하였다. 열처리 후 금도금층의 주 결정성장 방향은 XRD를 이용하여 측정하였다. 산처리에서 질산과 황산 중 질산에 의한 산화막제거 정도가 더 우수하게 나타났다. 활성화 처리시 zincate 용액을 희석시킬수록 입자 크기가 미세해 지고, 활성화 물질은 pH 13-13.5, 상온, 농도 15-25%의조건에서 크기가 작은 Zn 활성화 물질이 균일하게 분포하였다. Ni과 Auan전해도금 속도는 온도와 pH가 증가할수록 증가하였다. Ni 무전해 도금 조건은 pH 4.5, 온도 $90^{\circ}C$, 시간 20분이며, Au 무전해 도금조건은 pH7, 온도 $80^{\circ}C$, 시간 10분이었다. 상온에서 $400^{\circ}C$까지 30분동안 열처리 한 후 금도금막의 결정 방향은 pH 7, 온도 $80^{\circ}C$, 시간 10분이었다. 상온에서 $400^{\circ}C$까지 30분 동안 열처리 한 후 금도금막의 결정 방향은 pH 7에서 (111), pH 9에서는 (200)과 (111)이 주 peak로 나타났으며, 열처리에 의한 결정 방향의 변화는 없었다. 전체 공정에서 최종적인 표면 형상에 영향을 주는 단계는 활성화 처리로서 flip chip의 bonding layer형성에 가장 중요한 요소임을 알 수 있었다.보다 자생지(自生地)에서 높은 함량(含量)을 보였다. 5. 무기성분함양(無機成分含量)의 차이(差異)는 K의 경우(境遇) 자생지(自生地)에서 보다 재배지(栽培地)에서 평균적(平均的)으로 10배이상(倍以上) 정도(程度) 높은 함량(含量)의 차이(差異)를 보였으나 Mn, Zn, Na, Cu 등(等)은 일정(一定)한 경향(傾向)을 보이지 않는 것으로 나타났다. 6. 유리(遊離) 아미노산(酸)의 함량(含量)은 자생지(自生地은)보다 재배지(栽培地)에서 전반적(全般的)으로 높은 함량(含量)을 나타내었고, 특(特)히 Arginine은 다른 성분(成分)들과 비교(比較)해 볼 때 가장 높은 조성(組成)의 차이(差異)를 나타내었다. 7. 야생(野生)더덕과 재배(栽培)더덕의 정유성분수율(精油成分收率)은 자생지재배(自生地栽培)에서는 모두 0.004% 였고 재배지(栽培地)에서는 야생(野生)더덕이 0.005%였다. 8. 더덕의 재배장소(栽培場所)에 따른 향기성분(香氣成分)은 총(總) 21종(種)이었으며 自生地(自生地)에서 야생(野生)더덕은 16종(種), 재배(栽培)더덕은 18종(種)이었고, 재배지(栽培地)에서 야생(野生) 더덕은 14종(種), 재배(栽培)더덕은 20(種)이었다. 9. Trans-2-hexanol은 야생(野生)더덕의 자생지(自生地) 재배(栽培)에서 피이크 면적(面積) 당(當) 50.3%, 재배지(栽培地)에서 피이크 면적(面積) 당(當) 43.3%를 보였으며 amylalcohol, furfuryl acetate, 2-methoxy-4-vinyl phenol(MVP)는 재배(栽培)더덕에서만 확인(確認)되었다.는 KI, BMI와 유의적인 양의 상관관계를 보였고 (p<0.01), HCL-C은 비체중, BMI, LBM, TBM와 유의적인 음의 상관관계를 보였으며, (p<0.01), KI, SBP와도 음의 상관관계를 보였다. (p<0.05), LCL-C는 KI와 유의적이인 양의

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