대관령 지역에 많이 분포하고 있는 두 토양, 석비레(Saprolite) 토양과 차항통 (Chahang series) 토양을 사용하여 경사면이 균일한 나지 토양에서 경사도 0.5, 7, 15, 30%와 강우강도 20, 60, 90 mm hr<sup>...

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https://www.riss.kr/link?id=A99602972
2012
Korean
KCI등재
학술저널
877-881(5쪽)
4
0
상세조회0
다운로드대관령 지역에 많이 분포하고 있는 두 토양, 석비레(Saprolite) 토양과 차항통 (Chahang series) 토양을 사용하여 경사면이 균일한 나지 토양에서 경사도 0.5, 7, 15, 30%와 강우강도 20, 60, 90 mm hr<sup>...
대관령 지역에 많이 분포하고 있는 두 토양, 석비레(Saprolite) 토양과 차항통 (Chahang series) 토양을 사용하여 경사면이 균일한 나지 토양에서 경사도 0.5, 7, 15, 30%와 강우강도 20, 60, 90 mm hr<sup>-1</sup>의 조합으로 12처리를 하여 토양 유실에 대한 인공강우실험을 하였다. 그 결과를 요약하면 다음과 같다.
석비레 (Saprolite) 토양에서는 경사도 7% 까지는 토양유실이 적게 나타나다가 7% 이상의 경사면에서는 급격하게 증가하였고 차항통 (Chahang series) 토양은 경사도, 강우강도 증가와 함께 유실이 점증하였고, 경사도와 강우강도가 적은 조합에서도 유실이 다소 크게 나타났다. 경사도 15, 30%와 강우강도 60, 90mm/hr<sup>-1</sup>의 조합처리에서는 두 토양 모두 토양유실이 크게 일어나고, 두 토양 간에 큰 차이는 없었다.
차항통 (Chahang series) 토양은 경사도, 강우강도가 적은 조합에서도 유실이 일어날 위험성이 크므로 토양관리에 주의를 요한다.
다국어 초록 (Multilingual Abstract)
This research was carried out to investigate the interaction effect of slope gradient and rainfall intensity on soil loss with rainfall simulator. The soils used in this experiment were saprolite, Chahang series which distributed extensively in Daegwa...
This research was carried out to investigate the interaction effect of slope gradient and rainfall intensity on soil loss with rainfall simulator. The soils used in this experiment were saprolite, Chahang series which distributed extensively in Daegwanryong. Slope gradient applied was 0.5, 7, 15 and 30%. Rainfall intensity applied was 20, 60 and 90 mm hr<sup>-1</sup>. The result obtained can be summarised as follow; Overall, Chahang series suffered more losses than saprolite. Chahang series shows the immediately large increase of soil loss with the increasing soil gradient and rainfall intensity. However, saprolite shows a little increasing loss up to 7% gradient and abruptly increasing loss logarithmically over 7% gradient in soil slope. In combination of slope gradient 15, 30% and rainfall intensity 60, 90 mm hr<sup>-1</sup> processing, both soil erosion happened significantly. And there was no significant difference between the two soils. Because Chahang series have the danger of soil loss with low slope gradient and rainfall intensity, we should give greater attention to soil management in Chahang series.
참고문헌 (Reference)
1 Meyer, L.D., "Use of the rainulator for runoff plot research" 24 : 319-321, 1960
2 Posen, J., "The influence of slope angle on infiltration rate and Hortonian overland flow volume" 49 : 117-131, 1984
3 Duly, F.L., "The effect of the degree of slope on runoff and soil erosion" 45 : 352-360, 1932
4 De Ploey, J., "The differential impact of some soil loss factors on flow, runoff creep and rainwash" 151-161, 1976
5 Bouyoucos, G.J., "The cray ratio as a criterion of suceptibility of soils to erosion" 27 : 738-741, 1953
6 Whang, E., "Studies on the soil erosion of the various type bench terrace composed of the granite soil" 3 : 23-30, 1966
7 Woo, B.M., "Studies on the development of accelerating measures of establishment of vegetation on bare slopes" 24 : 1-24, 1974
8 Woo, B.M., "Studies on soil conservation effects of the straw-mat mulching (Ⅲ) - Effects of the mat structures and Its practicality" 27 : 5-14, 1975
9 Oh, W.K., "Soil Conservation and Maintenance of Fertility on Upland Soils" 6 (6): 53-60, 1973
10 Lehrsch, G.A., "Selection of a parameter describing soil surface roughness" 52 : 1439-1445, 1988
1 Meyer, L.D., "Use of the rainulator for runoff plot research" 24 : 319-321, 1960
2 Posen, J., "The influence of slope angle on infiltration rate and Hortonian overland flow volume" 49 : 117-131, 1984
3 Duly, F.L., "The effect of the degree of slope on runoff and soil erosion" 45 : 352-360, 1932
4 De Ploey, J., "The differential impact of some soil loss factors on flow, runoff creep and rainwash" 151-161, 1976
5 Bouyoucos, G.J., "The cray ratio as a criterion of suceptibility of soils to erosion" 27 : 738-741, 1953
6 Whang, E., "Studies on the soil erosion of the various type bench terrace composed of the granite soil" 3 : 23-30, 1966
7 Woo, B.M., "Studies on the development of accelerating measures of establishment of vegetation on bare slopes" 24 : 1-24, 1974
8 Woo, B.M., "Studies on soil conservation effects of the straw-mat mulching (Ⅲ) - Effects of the mat structures and Its practicality" 27 : 5-14, 1975
9 Oh, W.K., "Soil Conservation and Maintenance of Fertility on Upland Soils" 6 (6): 53-60, 1973
10 Lehrsch, G.A., "Selection of a parameter describing soil surface roughness" 52 : 1439-1445, 1988
11 Schmidt, H.L., "Relative erodibility of three loss derived soils" 28 : 570-577, 1964
12 Wischmeier, W.H., "Relation of soil properties to its erodibility" 33 : 131-137, 1969
13 Ellison, W.D., "Rainfall applicater" 25 : 22-23, 1944
14 Middleton, H.E., "Properties of soils which influence soil erosion" U.S.D.A 1930
15 Ekern, P.C., "Problems of raindrop impact erosin" 34 : 23-25, 1935
16 Wischmeier, W.H., "Predicting Rainfall Erosion Losses -A Guide to Conservation Planning. USDA Hand Book. 537" 1978
17 Mitchell, J.K., "Micro-relief surface depression storage: changes during rainfall events and their application to rainfall-runoff models" 14 : 777-802, 1978
18 Mitchell, J.K., "Micro-relief surface depression storage: analysis of models to describe depthstorage function" 12 : 1205-1222, 1976
19 Meyer, L.D., "Mathematical simulation of the process of soil erosion" 754-758, 1969
20 Emily, T. Essig, "Infiltration and deep flow over sloping surfaces: Comparison of numerical and experimental results" 374 : 30-42, 2009
21 Ribolzia, O., "Impact of slope gradient on soil surface features and infiltration on steep slopes in northern Laos" 127 : 53-63, 2011
22 Philip, J.R., "Hillslope infiltration; planar slopes" 27 (27): 109-117, 1991
23 Li Chen, "Green-Ampt infiltration model for sloping surfaces" 42 : 1-9, 2006
24 Govers, G., "Field study on topographical and topsoil effects on runoff generation" 18 : 91-111, 1991
25 Wischmeier, W.H., "Effect of organic matter content of the soil on infiltration" 20 : 150-152, 1965
26 Etse, S.K., "Determination and analysis of surface depression storage and overland flow of different tillage models as a function of slope and rainfall intensity" Agricultural University Wageningen 1987
27 Wischmeier, W.H., "A rainfall erosion index for a Universal soil loss equation" 23 : 246-249, 1959
토양 특성 및 토지이용에 따른 낙동강 상류지역 토양침식위험성 평가
면역크로마토그래피를 이용한 토양 및 쌀의 Cd 간이진단법 평가
전황함량과 순산발생능력의 상관관계를 통한 잠재특이산성토양 기준 설정
학술지 이력
| 연월일 | 이력구분 | 이력상세 | 등재구분 |
|---|---|---|---|
| 2026 | 평가예정 | 재인증평가 신청대상 (재인증) | |
| 2020-01-01 | 평가 | 등재학술지 유지 (재인증) | ![]() |
| 2017-01-01 | 평가 | 등재학술지 유지 (계속평가) | ![]() |
| 2013-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
| 2010-01-01 | 평가 | 등재 1차 FAIL (등재유지) | ![]() |
| 2008-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
| 2007-05-25 | 학술지명변경 | 한글명 : Korean Journal of Soil Science and Fertilizer -> 한국토양비료학회지(Korean Journal of Soil Science and Fertilizer) | ![]() |
| 2006-06-20 | 학술지명변경 | 한글명 : Korean Journal of Soil Science & Fertilizer -> Korean Journal of Soil Science and Fertilizer | ![]() |
| 2006-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
| 2003-01-01 | 평가 | 등재학술지 선정 (등재후보2차) | ![]() |
| 2002-01-01 | 평가 | 등재후보 1차 PASS (등재후보1차) | ![]() |
| 2000-07-01 | 평가 | 등재후보학술지 선정 (신규평가) | ![]() |
학술지 인용정보
| 기준연도 | WOS-KCI 통합IF(2년) | KCIF(2년) | KCIF(3년) |
|---|---|---|---|
| 2016 | 0.37 | 0.37 | 0.36 |
| KCIF(4년) | KCIF(5년) | 중심성지수(3년) | 즉시성지수 |
| 0.38 | 0.41 | 0.544 | 0.08 |