KCI등재
황폐임야가 수해참상에 미치는 영향 : 천보산과 인접 죽엽산을 중심으로 Observed at Chonbo and the neighbouring Mt . Jook - yop area = Influences of the devastated forest lands on flood damages
저자
정인구 (임업시험장)
발행기관
학술지명
권호사항
발행연도
1966
작성언어
Korean
KDC
526
등재정보
KCI등재
자료형태
학술저널
수록면
4-9(6쪽)
제공처
소장기관
1. On 13 September 1964 a storm raged for 3 hours and 20 minutes with pounding heavy rainfalls, and precipitation of 287.5 mm was recorded on that day.
The numerous landslides were occured in the eroded forest land neighbouring Mt. Chunbo, while no landslides recorde at all on Mt. Jookyup within the premise of Kwangnung Experiment Station, the Forest Experiment Station.
2. Small-scalled Landslides were occured in 43 different places of watershed area (21.97 ha.) in which the survey had already been done, in and around Mt. Chunbo (378 m a.s.l.).
The accumulated soil amount totaled 2,146,56 ㎥ due to the above mentioned landslides, while soil accumulated from riverside erosion has reached to 24,168.79 ㎥, consisting of soils, stones, and pebbles. However, no landslides were reported in the Mt. Jook yup area because of dense forest covers. The ratio of the eroded soil amount accumulated from the riversides to that of watershed area was 1 to 25.
On the other hand, the loss and damage in the research area of Mt. Chonbo are as follows:
28 houses completly destroyed or missing
7 houses partially destroyed
51 men were dead
5 missing, and 57 wounded.
It was a terrible human disaster
However, no human casualties were recorded at all, 1 house-completly destroyed and missing, 2 houses-partially destroyed.
Total : 3 houses were destroyed or damaged, in The area of Mt. Jookyup
3. In the calculation of the quanty of accumulated soil, the or mula of $quot;V=1/3h (a+√ab+b)$quot; was used and it showed that 24, 168.79m of soil, sands, stones and pebbles carried away.
4. Average slope of the stream stood 15 at the time of accident and well found that there was a correlation between the 87% of cross-area sufferd valley erosion and the length of eroded valley, after a study on regression and correlation of the length and cross-area.
In other works, the soil erosion was and severe as we approached to the down-stream, counting at a place of average (15。1′) and below.
We might draw a correlation such as $quot;Y=ax-b$quot; in terms of the length and cross-area of the eroded valley.
5. Sites of char-coal pits were found in the upper part of the desert-like Mt. Chunbo and a professional opinion shows that the mountain was once covered by the oak three species.
Furthermore, we found that the soil of both mountains have been kept the same soil system according to a research of the soil cross-area.
In other words, we can draw out the fact that, originally, the forest type and soil type of both Mt. Chunbo (378m) and Mt. Jookyup (610m) have been and are the same.
However, Mt. Chunbo has been much more devastated than Mt. Jookyup, and carried away its soil nutrition to the extent that the ratios of N. P₂O_5K₂O and Humus C.E.C between these two mountains are 1:10:1:5 respectively.
6. Mt. Chunbo has been mostly eroded for the past 30 years, and it consists of gravels of 2mm or larger size in the upper part of the mountain, while in the lower foot part, the sandy loam was formulated due to the fact that the gluey soil has been carried and accumulated.
On the hand, Mt. Jookyup has consitantly kept the all the same forest type and sandy loam of brown colour both in the upper and lower parts.
7. As for the capability of absorbing and saturating maximum humidity by the surface soil, the ratios of wet soil to dry soil are 42.8% in the hill side and lower part of the eroded Mt. Chunbo and 28.5% in the upper part.
On the contrary, Mt. Jookyup on which the forest type has not been changed, shows that the ratio in 77.4% in the hill-side and 68.2% in the upper part, approximately twice as much humidity as Mt. Chunbo.
This proves the fact that the forest lands with dense forest covers are much more capable of maintaining water by wood, vegitation, and an organic material.
The strength of dreventing from carring away surface soil is great due to the vigorous network of the root systems.
8. As mentioned above, the devastated forest land cause not only much greater devastation, but also human loss and property damage.
We must bear in mind that the eroded forest land has taken the valuable soil, which is the very existence of origin of both human being and all creatures.
As for the prescription for preventing erosion of forest land, the trees for furtilization has to be planted in the hill,side with at least reasonable amount of aertilizer, in order to restore the strength of earth soil, while in the lower part, thorough erosion control and reforestation, and establishments along the riversides have to be made, so as to restore the forest type.
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