• 한국농공학회지
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• 제17권1호
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• pp.3642-3654
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• 1975

The purpose of this thesis is to derive a unit hydrograph which may be applied to the ungaged watershed area from the relations between directly measurable unitgraph properties such as peak discharge(qp), time to peak discharge (Tp), and lag time (Lg) and watershed characteristics such as river length(L) from the given station to the upstream limits of the watershed area in km, river length from station to centroid of gravity of the watershed area in km (Lca), and main stream slope in meter per km (S). Other procedure based on routing a time-area diagram through catchment storage named Instantaneous Unit Hydrograph(IUH). Dimensionless unitgraph also analysed in brief. The basic data (1969 to 1973) used in these studies are 9 recording level gages and rating curves, 41 rain gages and pluviographs, and 40 observed unitgraphs through the 9 sub watersheds in Nak Oong River basin. The results summarized in these studies are as follows; 1. Time in hour from start of rise to peak rate (Tp) generally occured at the position of 0.3Tb (time base of hydrograph) with some indication of higher values for larger watershed. The base flow is comparelatively higher than the other small watershed area. 2. Te losses from rainfall were divided into initial loss and continuing loss. Initial loss may be defined as that portion of storm rainfall which is intercepted by vegetation, held in deppression storage or infiltrated at a high rate early in the storm and continuing loss is defined as the loss which continues at a constant rate throughout the duration of the storm after the initial loss has been satisfied. Tis continuing loss approximates the nearly constant rate of infiltration (${\Phi}$-index method). The loss rate from this analysis was estimated 50 Per cent to the rainfall excess approximately during the surface runoff occured. 3. Stream slope seems approximate, as is usual, to consider the mainstreamonly, not giving any specific consideration to tributary. It is desirable to develop a single measure of slope that is representative of the who1e stream. The mean slope of channel increment in 1 meter per 200 meters and 1 meter per 1400 meters were defined at Gazang and Jindong respectively. It is considered that the slopes are low slightly in the light of other river studies. Flood concentration rate might slightly be low in the Nak Dong river basin. 4. It found that the watershed lag (Lg, hrs) could be expressed by Lg=0.253 (L.Lca)0.4171 The product L.Lca is a measure of the size and shape of the watershed. For the logarithms, the correlation coefficient for Lg was 0.97 which defined that Lg is closely related with the watershed characteristics, L and Lca. 5. Expression for basin might be expected to take form containing theslope as {{{{ { L}_{g }=0.545 {( { L. { L}_{ca } } over { SQRT {s} } ) }^{0.346 } }}}} For the logarithms, the correlation coefficient for Lg was 0.97 which defined that Lg is closely related with the basin characteristics too. It should be needed to take care of analysis which relating to the mean slopes 6. Peak discharge per unit area of unitgraph for standard duration tr, ㎥/sec/$\textrm{km}^2$, was given by qp=10-0.52-0.0184Lg with a indication of lower values for watershed contrary to the higher lag time. For the logarithms, the correlation coefficient qp was 0.998 which defined high sign ificance. The peak discharge of the unitgraph for an area could therefore be expected to take the from Qp=qp. A(㎥/sec). 7. Using the unitgraph parameter Lg, the base length of the unitgraph, in days, was adopted as {{{{ {T}_{b } =0.73+2.073( { { L}_{g } } over {24 } )}}}} with high significant correlation coefficient, 0.92. The constant of the above equation are fixed by the procedure used to separate base flow from direct runoff. 8. The width W75 of the unitgraph at discharge equal to 75 per cent of the peak discharge, in hours and the width W50 at discharge equal to 50 Per cent of the peak discharge in hours, can be estimated from {{{{ { W}_{75 }= { 1.61} over { { q}_{b } ^{1.05 } } }}}} and {{{{ { W}_{50 }= { 2.5} over { { q}_{b } ^{1.05 } } }}}} respectively. This provides supplementary guide for sketching the unitgraph. 9. Above equations define the three factors necessary to construct the unitgraph for duration tr. For the duration tR, the lag is LgR=Lg+0.2(tR-tr) and this modified lag, LgRis used in qp and Tb It the tr happens to be equal to or close to tR, further assume qpR=qp. 10. Triangular hydrograph is a dimensionless unitgraph prepared from the 40 unitgraphs. The equation is shown as {{{{ { q}_{p } = { K.A.Q} over { { T}_{p } } }}}} or {{{{ { q}_{p } = { 0.21A.Q} over { { T}_{p } } }}}} The constant 0.21 is defined to Nak Dong River basin. 11. The base length of the time-area diagram for the IUH routing is {{{{C=0.9 {( { L. { L}_{ca } } over { SQRT { s} } ) }^{1/3 } }}}}. Correlation coefficient for C was 0.983 which defined a high significance. The base length of the T-AD was set to equal the time from the midpoint of rain fall excess to the point of contraflexure. The constant K, derived in this studies is K=8.32+0.0213 {{{{ { L} over { SQRT { s} } }}}} with correlation coefficient, 0.964. 12. In the light of the results analysed in these studies, average errors in the peak discharge of the Synthetic unitgraph, Triangular unitgraph, and IUH were estimated as 2.2, 7.7 and 6.4 per cent respectively to the peak of observed average unitgraph. Each ordinate of the Synthetic unitgraph was approached closely to the observed one.

• 생태와환경
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• 제45권2호
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• pp.158-173
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• 2012

본 연구는 대청호 본류유역 7개 지점과 대청호 유입지류 8개 지점을 선정하여 2001년부터 2010년까지 측정된 환경부 수질자료를 분석해 시 공간적 변이를 파악하고, 더불어 대청호 유입 지류에 의한 대청호 수질의 영향을 분석하였다. 본류 수역의 연평균 수질 자료 분석결과에 따르면, 질소(N) 및 인(P)의 농도는 호수대 내에서 상류역에서 댐(M7)으로 갈수록 거리에 따라 1차 함수적으로 감소하는 경향을 보였다. 호수내 유수대(M1~M3), 전이대(M4~M6) 및 정수대(M7)의 TN과 TP는 외국 인공호들과 마찬가지로 뚜렷한 Zonation 패턴을 보였다. 반면, 호수내 유기물 지표로서 엽록소(CHL)와 BOD는 TN과 TP의 구간별 연속적 감소 패턴과는 달리 전이대에서 최고치를 보였다. 유수대에서는 몬순 집중강우기인 8월에 TP가 377 ${\mu}gL^{-1}$로서 최대치를 보였으나, 정수대에서는 7월에 165 ${\mu}gL^{-1}$로서 최대치를 보였다. 한편, 유수대의 TN은 3월 최대치(8.52 $mg\;L^{-1}$)를 보였으며, 정수대의 TN은 본류에 비해 상대적으로 낮은 수치를 보였고, 최대치는 8월 (3.76 $mg\;L^{-1}$)에 관측되었다. 집중강우에 의한 이온희석현상은 9~10월에 극명하게 나타났다. 호수내 제한요인의 평가지표로서 이용되는 TN : TP 비는 88 이상으로서 이미 대청호는 질소가 과잉공급 상태인 것으로 사료되었다. 몬순강우에 따라 호수의 수질은 악화되는 경향을 보였으며, TP와 SS가 강우에 가장 민감하게 반응하였고, CHL은 정수대의 변이 폭이 높게 나타났다. 호수내로 유입되는 지천의 영향평가에 따르면, 도심형 하천이자 농공단지와 하수처리장의 영향을 받고 있는 T1, T2 및 호수내에 가장 큰 영향을 줄 것으로 사료되는 옥천천(T5)의 오염도가 가장 높게 나타났다. 호수의 경험적 모델 분석에 다르면, 호수내에서 CHL의 변이는 유수대($R_z$: $R_2$=0.044, p=0.264)와 전이대 ($T_z$: $R_2$=0.126, p=0.054)에서 TN에 의해 통계학적 유의성을 보이지 않았으나, 정수대($L_z$)에서 질소는 조류 생장에 억제효과($R_2$=0.458, p=0.032)를 가질 수 있는 것으로 나타났다. 한편, 유입 지천($I_w$)의 TN은 호수내($I_r$)의 CHL의 변이에 통계학적으로 유의성이 없는 것으로 나타났고($R_2$=0.258, p=0.110), 유입 지천($I_w$)의 TP는 호수내($I_r$)의 CHL의 변이에 통계학적으로 유의성이 있는 것으로 나타났다 ($R_2$=0.567, p=0.005). 즉, 지천의 TP 유입은 대청호의 조류 생장에 직접적으로 영향을 주는 것을 의미하였다. 한편, 대청호의 TN : TP 비는 지천의 TN보다는 TP에 의한 영향을 받는 것으로 나타나 결국 TN : TP 비는 직접적으로 인(P)의 농도에 의해 조절되는 것으로 나타났다. 따라서 호수내의 여름철 TP와 SS 유입을 최소화 시키고, 높은 인이 유입되는 도심형 하천(옥천천)의 수질 개선이 대청호의 수질 개선에 큰 도움을 줄 것으로 사료되었다.

• Journal of the Korean Wood Science and Technology
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• 제2권4호
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• pp.4-14
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• 1974

The total forest land area in Korea accounts for some 67 percent of the nation's land total. Its productivity, however, is very low. Consequently, forest production accounts for only about 2 percent of the gross national product and a minor proportion of no more than about 5 percent versus primary industry. In this case, however, only the direct income from forestry is taken into account, making no reference to the forestry output induced by other industrial sectors. The value added Or the induced forestry output in manufacturing the primary wood products into higher quality products, makes a larger contribution to the economy than direct contribution. So, this author has tried to analyze the structure of forestry and compute the repercussion effect and the induced output of primary forest products when utilized by other industries for their raw materials, Hsing the input-output table and attached tables for 1963 and 1966 issued by the Bank of Korea. 1. Analysis of forestry structure A. Changes in total output Durng the nine-year period, 1961-1969, the real gross national product in Korea increased 2.1 times, while that of primary industries went up about 1. 4 times. Forestry which was valued at 9,380 million won in 1961, was picked up about 2. 1 times to 20, 120 million won in 1969. The rate of the forestry income in the GNP, accordingly, was no more than 1.5 percent both in 1961 and 1962, whereas its rate in primary industries increased 3.5 to 5.4 percent. Such increase in forestry income is attributable to increased forest production and rise in timber prices. The rate of forestry income, nonetheless, was on the decrease on a gradual basis. B. Changes in input coefficient The input coefficient which indicates the inputs of the forest products into other sectors were up in general in 1966 over 1963. It is noted that the input coefficient indicating the amount of forest products supplied to such industries closely related with forestry as lumber and plywood, and wood products and furniture, showed a downward trend for the period 1963-1966. On the other hand, the forest input into other sectors was generally on the increase. Meanwhile, the input coefficient representing the yolume of the forest products supplied to the forestry sector itself showed an upward tendency, which meant more and more decrease in input from other sectors. Generally speaking, in direct proportion to the higher input coefficient in any industrial sector, the reinput coefficient which denotes the use of its products by the same sector becomes higher and higher. C. Changes in ratio of intermediate input The intermediate input ratio showing the dependency on raw materials went up to 15.43 percent m 1966 from 11. 37 percent in 1963. The dependency of forestry on raw materials was no more than 15.43 percent, accounting for a high 83.57 percent of value added. If the intermediate input ratio increases in any given sector, the input coefficient which represents the fe-use of its products by the same sector becomes large. D. Changes in the ratio of intermediate demand The ratio of the intermediate demand represents the characteristics of the intermediary production in each industry, the intermediate demand ratio in forestry which accunted for 69.7 percent in 1963 went up to 75.2 percent in 1966. In other words, forestry is a remarkable industry in that there is characteristics of the intermediary production. E. Changes in import coefficient The import coefficient which denotes the relation between the production activities and imports, recorded at 4.4 percent in 1963, decreased to 2.4 percent in 1966. The ratio of import to total output is not so high. F. Changes in market composition of imported goods One of the major imported goods in the forestry sector is lumber. The import value increased by 60 percent to 667 million won in 1966 from 407 million won in 1963. The sales of imported forest products to two major outlets-lumber and plywood, and wood products and furniture-increased to 343 million won and 31 million won in 1966 from 240million won and 30 million won in 1963 respectively. On the other hand, imported goods valued at 66 million won were sold to the paper products sector in 1963; however, no supply to this sector was recorded in 1963. Besides these major markets, primary industries such as the fishery, coal and agriculture sectors purchase materials from forestry. 2. Analysis of repercussion effect on production The repercussion effect of final demand in any given sector upon the expansion of the production of other sectors was analyzed, using the inverse matrix coefficient tables attached to the the I.O. Table. A. Changes in intra-sector transaction value of inverse matrix coefficient. The intra-sector transaction value of an inverse matrix coefficient represents the extent of an induced increase in the production of self-support products of the same sector, when it is generated directly and indirectly by one unit of final demand in any given sector. The intra-sector transaction value of the forestry sector rose from 1.04 in 1963 to 1, 11 in 1966. It may well be said, therefore, that forestry induces much more self-supporting products in the production of one unit of final demand for forest products. B. Changes in column total of inverse matrix coefficient It should be noted that the column total indicates the degree of effect of the output of the corresponding and related sectors generated by one unit of final demand in each sector. No changes in the column total of the forestry sector were recorded between the 1963 and 1966 figures, both being the same 1. 19. C. Changes in difference between column total and intra-sector transaction amount. The difference between the column total and intra-sector transaction amount by sector reveals the extent of effect of output of related industrial sector induced indirectly by one unit of final demand in corresponding sector. This change in forestry dropped remarkable to 0.08 in 1966 from 0.15 in 1963. Accordingly, the effect of inducement of indirect output of other forestry-related sectors has decreased; this is a really natural phenomenon, as compared with an increasing input coefficient generated by the re-use of forest products by the forestry sector. 3. Induced output of forestry A. Forest products, wood in particular, are supplied to other industries as their raw materials, increasng their value added. In this connection the primary dependency rate on forestry for 1963 and 1966 was compared, i. e., an increase or decrease in each sector, from 7.71 percent in 1963 to 11.91 percent in 1966 in agriculture, 10.32 to 6.11 in fishery, 16.24 to 19.90 in mining, 0.76 to 0.70 in the manufacturing sector and 2.79 to 4.77 percent in the construction sector. Generally speaking, on the average the dependency on forestry during the period 1963-1966 increased from 5.92 percent to 8.03 percent. Accordingly, it may easily be known that the primary forestry output induced by primary and secondary industries increased from 16, 109 million won in 1963 to 48, 842 million won in 1966. B. The forest products are supplied to other industries as their raw materials. The products are processed further into higher quality products. thus indirectly increasing the value of the forest products. The ratio of the increased value added or the secondary dependency on forestry for 1963 and 1966 showed an increase or decrease, from 5.98 percent to 7.87 percent in agriculture, 9.06 to 5.74 in fishery, 13.56 to 15.81 in mining, 0.68 to 0.61 in the manufacturing sector and 2.71 to 4.54 in the construction sector. The average ratio in this connection increased from 4.69 percent to 5.60 percent. In the meantime, the secondary forestry output induced by primary and secondary industries rose from 12,779 million Wall in 1963 to 34,084 million won in 1966. C. The dependency of tertiary industries on forestry showed very minor ratios of 0.46 percent and 0.04 percent in 1963 and 1966 respectively. The forestry output induced by tertiary industry also decreased from 685 million won to 123 million won during the same period. D. Generally speaking, the ratio of dependency on forestry increased from 17.68 percent in 1963 to 24.28 percent in 1966 in primary industries, from 4.69 percent to 5.70 percent in secondary industries, while, as mentioned above, the ratio in the case of tertiary industry decreased from 0.46 to 0.04 percent during the period 1963-66. The mining industry reveals the heaviest rate of dependency on forestry with 29.80 percent in 1963 and 35.71 percent in 1966. As it result, the direct forestry income, valued at 8,172 million won in 1963, shot up to 22,724 million won in 1966. Its composition ratio lo the national income rose from 1.9 percent in 1963 to 2.3 per cent in 1966. If the induced outcome is taken into account, the total forestry production which was estimated at 37,744 million won in 1963 picked up to 105,773 million won in 1966, about 4.5 times its direct income. It is further noted that the ratio of the gross forestry product to the gross national product. rose significantly from 8.8 percent in 1963 to 10.7 percent in 1966. E. In computing the above mentioned ratio not taken into consideration were such intangible, indirect effects as the drought and flood prevention, check of soil run-off, watershed and land conservation, improvement of the people's recreational and emotional living, and maintenance and increase in the national health and sanitation. F. In conclusion, I would like to emphasize that the forestry sector exercices an important effect upon the national economy and that the effect of induced forestry output is greater than its direct income.

• 한국작물학회지
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• 제34권s02호
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• pp.45-65
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• 1989

우리나라는 지형과 기후가 복잡다양한 데다가 하절기에는 필리핀 남양군도로부터 상습적으로 불어오는 태풍의 진로권내에 위치해 있고 년간 강우량의 대부분이 벼 재배기인 하절기에 집중적으로 내리는 관계로 이때 강우와 강풍이 단독 또는 동반하여 갖가지 풍수해양상을 일으킨다. 풍해는 조풍해, 건조풍해 및 강풍해로 구분하여 볼 때 조풍해(염풍해)는 1986년 8월 28~29일 태품 Vera호 내습시 남부 해안지방 일대에서는 강우가 그치면서 염분을 함유한 초속 6m정도의 강풍이 불어 해안으로부터 2.5km까지 도체 조기에 염분을 건물당 1.1~17.2mg 부착시켜 심한 조풍해를 일으켰다. 그리고 건조풍해는 '87년 이래로 내습한 대부분의 태풍들이 4.0~8.5m의 태풍이 남부 및 동해안에 불어 Foenhn 현상으로 건조풍이 되고 이때 출수기에 처한 벼 이삭은 심한 백수피해와 변색위피해를 받았다. 태풍해로서는 풀수기 이전의 벼 생육단계에서 경엽이 기계적으로 절상, 파열, 고사되고, 등숙기에는 도복과 탈입이 심하게 된다. 풍해경감은 태품 내습을 회피하도록 8월 15일까지 출수시키고 풍해저항성이 비교적 강한 상풍벼와 청청벼 재배가 효과적이다. 한편 수해로서는 농경지 유시, 이몰, 침관수 및 도복 등을 들 수 있으나 각종 Dam, 제방축조, 하구언공사 등으로 피해는 많이 줄었지만 국지적 집중호우나 강변유역 제방내의 내수로 인한 침관수나 도복피해는 상습적으로 일어난다. 핌관수해는 태풍과 다우가 주로 8월 말경에 내습하여 2~4일 정도 도체가 관수된다. 이따 남부 특수만식답의 벼생육단계는 생육초중기에 해당되므로 어린 생육단게일수록 피해가 크고 보통식세어는 생식생장기에 해당되므로 유수나 팬이삭은 불념이 되더라도 죽은 이삭을 갖는 경의 상위절로부터 재생경이 나와 정상이삭으로 되어 수량 감소가 가장 튼 감수분열기 피해에서도 66%의 수량보상력을 갖게 된다. 침관수피해 경감을 위해서는 사전적 조처로서 관수저항성 및 백엽고, 벼멸구, 도복저항성을 갖는 품종을 선택 재배하는 것이 효과적이다. 특히 통일형 품종은 일본형 품종에 비하여 관수시 모든 생육단게에서 관수저항성이 강한데 묘생존율이 높고, 엽신과 엽초의 이상신장력이 낮아 퇴수시 기술적 장해가 적으며 생식생장기에는 근활력, 광합성능력이 높아 피해회복이 빠르고 고위절분얼이삭에 의한 수량보상력이 높다. 이상을 종합하여 볼 때 풍수해를 최소화하기 위해서는 다음과 같은 연구가 금후 이루어져야 할 것이다. \circled1 기상예보, 풍수해 피해실태 및 그로 인한 작황 등의 원격탐사 및 전산화에 의한 분석 연구가 이루어져야 하고, \circled2 품수해와 관련된 불량환경에서 내성을 갖는 품종 육성 보급이 이루어져야 하고, \circled3 품수해 발생상습지에서는 벼 피해를 보상할 수 있는 타작물과의 함리적 작부체계 개선 연구가 이루어져야 하고, \circled4 피해도체의 활용도 증진 연구가 이루어져야 할 것이다.

• Journal of Oral Medicine and Pain
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• 제31권4호
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• pp.297-316
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• 2006

의료분쟁 증가는 하나의 사회현상으로 특히, 인터넷을 통한 의료사고와 관련된 정보의 생산과 유통이 급속도로 증가되고 있는 현상을 간과해서는 안 된다. 본 연구는 2006년 3월 기준으로 인터넷 야후 포털 사이트에서 '의료사고'를 검색어로 하여 검색된 의료사고 관련 정보를 제공하는 웹사이트 28개를 사이트 개설자별로 분류하고 사이트 구성내용을 분석하여 의료사고 관련 사이트들의 현황과 개선되어야 할 문제점들을 비교 점검한 후 올바른 의료분쟁 해결을 위한 발전 방향을 모색하는 것을 연구목적으로 하여 분류항목별 전체 개수에 대한 비율을 조사한 결과 다음과 같은 결과를 얻었다. 1. 용어의 선호도에서 의료인, 일반인, 법조인 모두 '의료사고'라는 용어에 가장 익숙하거나 이를 선호하는 것으로 나타났다. 2. '의료사고' 검색어로 검색된 개설자별 사이트 개수를 비교한 결과 28개 사이트 중 의료인 4개, 일반인 7개, 법조인 17개였다. 의료인 중 치과의사가 개설한 사이트는 단지 1개였다. 3. 진료기록부 분석원을 따로 둔 일반인과 법조인 개설 사이트의 비율은 높았으며 치과관련 부분은 전무하였다. 4. 일반인은 의료사고 예방법에, 법조인은 의료사고 발생 이후 처리 과정에 주된 관심을 갖고 있는 것으로 보였으며, 이에 반해 의료사고 대책에 관해서 의료인 개설 사이트는 비중이 적은 것을 관찰할 수 있었다. 5. 일반인은 의료사고 발생시 대책으로 정부가 주도하는 공정한 제3자의 개입을 희망하는 것으로 조사되었다. 6. 개설자별 비교에서 의료인 개설 사이트는 의료사고에 대한 실례를 다른 개설 사이트에 비해 적게 다루는 것으로 나타났다. 7. 의료사고 상담글에서 치과 관련 내용이 많은 것에 비해 실제 판례 소개는 미미한 것으로 나타났다. 8. 국내 치과 판례 중 관혈적인 치과 치료에 대한 판례글이 많았던 반면 국내 공개 상담글은 비보험관련 치과 치료에 대한 상담글이 많았다. 9. 개설자별 의료사고 관련 정보 제공 게시판 글의 비교에서 일반인은 관련 용어, 의료인은 관련 의학지식, 법조인은 관련 법률에 대한 내용이 많았다. 10. 의료인, 일반인, 법조인 개설 사이트 모두 국내 의료사고 현황을 제공하는 형태로 언론보도 자료를 주로 사용하였으며, 일반인 개설 사이트 중 특히, 시민단체에서는 의료사고 관련 통계자료를 비중있게 다루고 있었다. 11. 적기는 하지만 의료사고 관련 사건을 수집하는 배너가 존재하는 사이트도 있었다. 이상의 결과를 볼 때 범람하는 정보들 속에서 제3자의 그릇된 정보로 의료분쟁 발생률이 증가될 소지가 크지만 의료인은 의료사고에 대해 가장 소극적인 것으로 나타나 이에 대해 향후 법조인-의료인, 환자-의료인, 일반인-의료인간의 상호대화와 정보교류를 통한 올바른 이해를 바탕으로 의료분쟁을 보다 적극적이고 능동적으로 조정, 해결하려는 노력을 보여야 할 것으로 사료된다.

• 동굴
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• 제68호
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• pp.23-73
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• 2005

Purpose of study; The purpose of this study is specifically classified as two parts. The one is to attempt the chronological annals of Quaternary topographic surface through the study over the formation process of alluvial surfaces in our country, setting forth the alluvial surfaces lower-parts of Han River area, as the basic deposit, and comparing it to the marginal landform surfaces. The other is to attempt the classification of micro morphology based on the and condition premising the land use as a link for the regional development in the lower-parts of Han river area. Reasons why selected the Lower-parts of Han river area as study objects: 1. The change of river course in this area is very serve both in vertical and horizontal sides. With a situation it is very easy to know about the old geography related to the formation process of topography. 2. The component materials of gravel, sand, silt and clay are deposited in this area. Making it the available data, it is possible to consider about not oかy the formation process of topography but alsoon the development history to some extent. 3. The earthen vessel, a fossil shell fish, bone, cnarcoal and sea-weed are included in the alluvial deposition in this area. These can be also valuable data related to the chronological annals. 4. The bottom set conglometate beds is also included in the alluvial deposits. This can be also valuable data related to the research of geomorphological development. 5. Around of this area the medium landform surface, lower landform surface, pediment and basin, are existed, and these enable the comparison between the erosion surfaces and the alluvial surfaces. Approach : 1. Referring to the change of river beds, I have calculated the vertical and horizontal differences comparing the topographic map published in 1916 with that published in 1966 and through the field work 2. In classifying the landform, I have applied the method of micro morphological classification in accordance with the synthetic index based upon the land conditions, and furthermore used the classification method comparing the topographic map published in 1916 and in that of 1966. 3. I have accorded this classification with the classification by mapping through appliying the method of classification in the development history for the field work making the component materials as the available data. 4. I have used the component materials, which were picked up form the outcrop of 10 places and bored at 5 places, as the available data. 5. I have referred to Hydrological survey data of the ministry of Construction (since 1916) on the overflow of Han-river, and used geologic map of Seoul metropolitan area. Survey Data, and general map published in 1916 by the Japanese Army Survbey Dept., and map published in 1966 by the Construction Research Laboratory and ROK Army Survey Dept., respectively. Conclusion: 1. Classification of Morphology: I have added the historical consideration for development, making the component materials and fossil as the data, to the typical consideration in accordance with the map of summit level, reliefe and slope distribution. In connection with the erosion surface, I have divided into three classification such as high, medium and low-,level landform surfaces which were classified as high and low level landform surfaces in past. furthermore I have divided the low level landform surface two parts, namely upper-parts(200-300m) and bellow-parts(${\pm}100m$). Accordingly, we can recognize the three-parts of erosion surface including the medium level landform surface (500-600m) in this area. (see table 22). In condition with the alluvial surfaces I have classified as two landform surfaces (old and new) which was regarded as one face in past. Meamwhile, under the premise of land use, the synthetic, micro morphological classification based upon the land condition is as per the draw No. 19-1. This is the quite new method of classification which was at first attempted in this country. 2. I have learned that the change of river was most severe at seeing the river meandering rate from Dangjung-ni to Nanjido. As you seee the table and the vertical and horizontal change of river beds is justly proportionable to the river meandering rate. 3. It can be learned at seeing the analysis of component materials of alluvial deposits that the component from each other by areas, however, in the deposits relationship upper stream, and between upper parts and below parts I couldn't always find out the regular ones. 4. Having earthern vessel, shell bone, fossil charcoal and and seaweeds includen in the component materials such as gravel, clay, sand and silt in Dukso and Songpa deposits area. I have become to attempt the compilation of chronicle as yon see in the table 22. 5. In according to hearing of basemen excavation, the bottom set conglomerate beds of Dukso beds of Dukso-beds is 7m and Songpa-beds is 10m. In according to information of dredger it is approx. 20m in the down stream. 6. Making these two beds as the standard beds, I have compared it to other beds. 7 The coarse sand beds which is covering the clay-beds of Dukso-beds and Nanjidobeds is shown the existence of so-called erosion period which formed the gap among the alluvial deposits of stratum. The former has been proved by the sorting, bedding and roundness which was supplied by the main stream and later by the branch stream, respectively. 8. If the clay-beds of Dukeo-bed and Songpa-bed is called as being transgressive overlap, by the Eustatic movement after glacial age, the bottom set conglomerate beds shall be called as being regressive overlap at the holocene. This has the closest relationship with the basin formation movement of Seoul besides the Eustatic movement. 9. The silt-beds which is the main component of deposits of flood plain, is regarded as being deposited at the Holocene in the comb ceramic and plain pottery ages. This has the closest relationship with the change of river course and river beds.