• Proceedings of the Plant Resources Society of Korea Conference
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• 2019.04a
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• pp.59-59
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• 2019

벼룩이울타리(Arenaria juncea M.Bieb.)는 7~8월에 백색의 꽃이 취산화서로 아름답게 피며, 산지, 산비탈 또는 메마른 초지에 자생한다. 청열 및 양혈의 효능이 있고, 은시호의 대용으로 쓰이며, 뿌리에는 triterpenoid saponins과 sapogenin이 함유되어 있다. 본 연구는 분화용 식물로 벼룩이울타리를 활용하기 위한 효율적인 포트 정식방법을 개발하기 위하여 수행되었다. 실험은 2018년 선행연구에서 생산된 유묘를 7월 2일에 정식하여 10월 15일까지 약 15주 동안 재배하였다. 대조구는 플라스틱 화분 10호($9{\times}9cm$)에 원예상토를 충진하고 200구 트레이에 셀 당 4립씩 파종하여 생산된 1셀을 정식하였다. 재배 실험은 용기종류[비닐포트(3, 4치), 플라스틱 포트(8, 10, 12호)], 토양 종류[원예상토, 중화 피트모스:펄라이트(3:1, 4:1), 마사토:중화 피트모스(2:1, 3:1)], 묘의 소질[파종 립수(1, 2, 4, 6립), 파종 용기(162, 200, 288구 트레이)] 등을 달리하여 진행하였다. 연구의 결과, 벼룩이울타리는 토양의 양이 많을수록 생육이 양호한 결과를 보여, 플라스틱 12호에 재배하는 것이 분화용으로 가장 효과적이었다. 한편, 비닐 4치와 플라스틱 10호의 경우, 플라스틱 12호와 생육에 큰 차이가 없어 경제적인 것으로 판단된다. 벼룩이울타리는 원예상토에서 재배하는 것이 전반적으로 생육이 우수하였으며, 다음으로 마사토와 피트모스 혼용토 순이었다. 그러나 피트모스와 펄라이트 혼용토는 비율과 관계없이 생육이 감소하며, 잎에 황백화 현상이 나타났다. 셀당 파종량을 달리하여 육묘한 후 정식한 결과, 전반적인 생육은 1립 파종묘에서 양호하였으나, 2, 4, 6립 파종묘가 1립 처리구에 비해 포트당 엽수가 약 1.35, 1.44, 2.01배 증가하는 경향을 보였다. 그러므로 유묘 생산시 셀당 파종량을 늘려 재배하는 것이 분화용으로 효과적일 것으로 판단된다. 파종용기별 유묘의 생육은 162, 200, 288구 트레이 순이었으나, 정식 후 약 15주 동안 재배한 결과, 162, 200구에서 생산된 유묘를 정식하는 것이 288구보다 양호하였다. 따라서, 육묘 단계에서 토양 및 공간을 절약할 수 있는 200구에 파종하여 재배하는 것이 효율적인 방법으로 생각된다. 결론적으로, 벼룩이울타리의 분화용 재배는 플라스틱포트 12호에 원예상토를 충진하고 200구 트레이에 4립 또는 6립을 파종하여 육묘한 묘를 정식하는 것이 가장 효과적이다. 한편, 경제적인 측면을 고려할 때, 재배면적을 적게 차지하는 비닐포트 4치 또는 플라스틱 포트 10호에 마사토와 중화 피트모스를 혼용하여 충진한 다음 유묘를 이식하는 것도 하나의 방법으로 판단된다.

• Journal of Korea Water Resources Association
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• v.55 no.4
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• pp.291-300
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• 2022

Artificial disturbance in mountainous areas increases the sensitivity to erosion by exposure of the subsoil with a low loam ratio to the surface. In this study, rainfall simulations were conducted to evaluate the erodibility of sand and loamy sand in the interrill erosion by the rainfall-induced sheet flow. The mean diameters of sand and loamy sand used in the experiment were 0.936 mm and 0.611 mm, respectively, and the organic matter content was 2.0% and 4.2%, respectively. In the experimental plot, the runoff coefficient of overland flow increased 1.16 times in loamy sand rather than sand. Mean sediment yields of loamy sand and sand by sheet erosion were 3.71kg/m²/hr and 1.13kg/m²/hr respectively. The erodibility, the rate of soil erosion for rainfall erosivity factor, was 3.65 times greater in loamy sand than in sand. As the gradient of the steep slope increased from 24° to 28°, the sediment concentration and the erodibility for two soils increased by about 20%. The erodibility factor K of sandy soils for small plots was overestimated compared to the measured erodibility. This means that RUSLE can overestimate the sediment yields by sheet erosion on sandy soils.

• Journal of The Korean Society of Grassland and Forage Science
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• v.18 no.3
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• pp.223-232
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• 1998

The main experiment related to this report was undertaken to assess the effects of two rates of $Ca(OH)_2$ (0, 250 kg/10a only at establishment) and five rates of $N-P_20_5-K_20$ (0-0-0, 0-10-10, 6-15-15, 12-20-20, 24-25-20 kg/10a/year) on the pasture establishment, forage yield and quality, and vegetation etc. After this 10-year main e experiment pasture had been used to assess the effects of the above treaments on the soil characteristics in oversown hilly pasture of a grass-clover sward. soil properties of mutual ratios of exchangeable cations at d different soil depth, and the visible characteristics of soil conservation obtained are summarized as follows; 1. Compared with the properties of soil fertility and the level for the likelihood grass tetany, the mutual ratios of exchangeable cations in soils; Ca:Mg:K(% of CEC), Ca:Mg:K(K=I), $K/\sqrt{Ca+Mg}$, Mg/K, K/Mg, and Ca/Mg, were discussed at different soil depth. Before and after experiment, these ratios were generally unbalance and unsuitable, and were rather worsened in the order of Mg>Ca>K under the conditions of liming and NPK fertilization without Mg. 2. The ratios of Ca and Ca/Mg were increaby liming, whereas it of $K/\sqrt{Ca+Mg}$ was redused. The ratios of K and $K/\sqrt{Ca+Mg}$ in control and the heavy fertillization of NPK(especially N) were rather lowered than those in the low and medium fertilizations of NPK. 3. The prperties of consevation were closely related with the forage productivity/vegetation rates, as affected by liming and the application rates of NPK. In control of NPK, It was shown to be the worst soil conservation; severly eroded(3rd grade), exporsure of subsoil, redish brown in soil colour, and 18.8% of cobble and stony in covering rate. 4. The improvement of soil conservation was greatly enhanced by increasing the NPK rate. In the medium and heavy fertilizations of NPK, it was shown to be the favorable improvement of soil conservation; slightly eroded(lst grade), covered with humus layer/grass residues in surface soil, dark brown in surface soil colour, under 1% of cobble and stony in covering rate. The increasing of legume yield/vegetation rate by liming rather enhanced the soil conservation of grassland.

• Journal of Korean Society of Forest Science
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• v.88 no.4
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• pp.498-509
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• 1999

This study aims to clarify the effect of forest management practices(thinning and pruning) in forest hydrological processes on electrical conductivity to get the fundamental information on the facilitation of purifying water quality after forestry practices. Rainfall, throughfall, stemflow, soil and stream water were sampled at the study sites which consist of Abies holophylla and Pinus koraiensis in Kwangnung Experimental Forest for 6 months from March 1 to August 4, 1998. In case of deviding into forest hydrological processes, multiple regression equations of electrical conductivity and total amount of anion, $NO{_3}^-$ of throughfall, stemflow, soil water of management site in Abies holophylla shows high significance. And multiple regression equations of electrical conductivity and total amount of anion, $SO{_4}^{2-}$, $Cl^-$ of throughfall, stemflow, soil water of non-management site in Abies holophylla shows high significance. Multiple regression equations of electrical conductivity and $NO{_3}^-$, before non-rain days of throughfall, stemflow, soil water of management site in Pinus koraiensis shows high significance. And multiple regression equations of electrical conductivity and total amount of ion, $NO{_3}^-$, $K^+$, pH, total amount of anion of throughfall, stemflow, soil water of non-management site in Plinus koraiensis shows high significance. Multiple regression equations of electrical conductivity and pricipitation, total amount of ion, $Na^+$ of stream water in Abies holophylla and Pinus koraiensis shows high significance. In case of combining into forest hydrological processes, multiple regression equations of electrical conductivity and total amount of cation and anion, $Na^+$, $Cl^-$, and pH in rainfall, throughfall, stemflow, soil and stream water shows high significance.

• Journal of Sericultural and Entomological Science
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• v.16 no.1
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• pp.1-20
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• 1974

These studies are conducted to find out inducing factors for the non-sprouting bud which appears in the utility reclaimed hill mulberry held and to establish control method for it since 1971. The results are as follows： 1. In spring, winter bud does not germinate at all on the top of branches or does wither suddenly after or during its germination. Necrosis and browning are appeared in cortex and phloem of non-sprouting bud branch. In autumn, the deterioration of leaves, the abnormal leaves on the top of branch, and browning of veins or petioles are also observed. 2. The soil of non-sprouting bud mulberry Held were found to be sand loom derived from granite rocks. The sub soil of it was very poor in development of root system because it had hard soil and lower pore space ratio. Especially, the sub soil to bring about severe non-sprouting bud had been easily appeared with deficiency of moisture content because of high density solid. 3. Content of soil moisture was significantly lower in the severe non-sprouting bud soil than in the healthy field. The sub soil o( the healthy field contained proper moisture content. On the other hand, the sub soil of the severe non-sprouting bud held contained almost critical moisture content for wilting. 4. The depth of available soil was shallow in the non-sprouting bud than in the healthy fold. The more rate of the non-sprouting bud was severe, the more available soil depth was sallow. 5. Available boron content in soil was affected by moisture content in soil. There was. lower moisture content in the non-sprouting bud field than that in healthy fold during 5, June to 5, September. 6. There was no significant correlation between soil pH and available boron content. On the other hand, the correlation of the content of organic matter and available boron content appeared to be highly positive significance. 7. The quantity of boron was significantly contained more in healthy mulberry field (0.34∼0.43ppm) than in non-sprouting bud field (0.10∼0.28ppm). 8. Boron content in leaves and barks was significantly lower in the non-sprouting bud trees than in healthy trees. 9. The symptom of non-sprouting bud induced from boron free sand culture was similar with that arised in the non-sprouting bud field. 10. The rate of non-sprouting bud was high by the increased application of lime. Considering the facts mentioned the above, author may conclude that the non-sprouting bud of mulberry tree is caused by boron deficiency, but also it is affected by the parent rocks, organic matter, soil moisture content and lime application. 11. The non$.$sprouting bud may be completely controlled by the application of 6∼9kg borax per 10a mulberry field twice a year in spring and summer.

• 한국공간정보시스템학회:학술대회논문집
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• 2007.06a
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• pp.436-440
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• 2007

ArcView와 연동하는 SWAT(Soil and Water Assessment Tool)은 수문평가 도구로써 사용되는 모형이다. 이러한 SWAT모형은 유역의 서로 다른 표면 특성을 반영할 수 있도록 대상유역을 몇 개의 소유역으로 나누고 소유역 내에서 유사한 특성을 나타내는 HRU으로 세분화한다. 모형에서는 유역부분과 수체부분으로 나누어 모의가 이루어지며 각 소유역에서 물수지식에 따라 강우량, 지하수로의 침투량, 증발산량, 그리고 표면 유출량을 산정한다. SWAT 모형은 많은 입력 자료가 있으며 그 중에서도 소유역 개수와 HRU개수가 SWAT 모형의 결과에 많은 영향을 미칠 것으로 생각되어 본 논문에서는 이에 대한 영향을 분석하였다. 연구 대상지역은 함평천 유역으로 전라남도 함평군과 무안군 사이에 위치하고 있으며 유역의 면적은 $196.4km^2$이고 유역의 대부분이 산지와 농업지역으로 이루어져 있다. SWAT 모형을 모의하기 위한 지형자료는 1:25,000 수치지도, 농업과학기술원의 1:25,000 정밀토양도, 환경부의 토지피복도를 사용하였고 기상자료와 강우자료는 목포기상관측소의 자료를 사용하였다. 매개변수를 추정하기위해 환경부의 오염총량관리 세유역을 사용하였으며 모의 결과를 실측치와 비교함으로서 매개변수를 추정하였다. 추정된 매개변수를 이용하고 연구대상지역의 소유역 개수와 HRU개수를 여러 가지로 변화시켜 모의하였으며 그 결과를 실측치와 비교하여 최적 소유역 개수와 HRU 개수를 추정하였다. 본 연구의 결과는 SWAT모형 수행시 소유역의 면적에 대한 객관적인 기준을 제시할 수 있을 것이다.

• Magazine of the Korean Society of Agricultural Engineers
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• v.39 no.2
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• pp.113-123
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• 1997

This study was initiated to build runoff plots, install soil and water quality monitoring systems and collect background data from the plots and neighboring soils as the 1st year study of a 5 year project to assess soil quality and develop the management practices for environmentally sound agriculture in mountainous soils. Eleven $3{\times}15m$ runoff plots and monitoring systems were installed at a field of National Alpine Agricultural Experiment Station to monitor soil quality and discharge of nonpoint source pollutants. Corn and potato were cultivated under different fertilizer, tillage and residue cover treatments. The soil has a single-layered cluster structure that has a relatively good hydrologic properties and can adsorb a large amount of nutrient. Concentrations of T-N, $NH_4$-N, and $NO_3$-N of surface soil sampled in the winter were relatively high. Runoff quality in the winter and thawing season in the spring was largely dependent on surface freezing, snow accumulation, temperature, surface thawing depth and so on. Runoff during the thawing season caused serious soil erosion but runoff quality during the winter was relatively good. Serious wind erosion from unprotected fields after the fall harvest were obserbed and best management practices to reduce the erosion need to be developed.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.234-238
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• 2008

The energy conservation theory is introduced for investigating processes of runoff and soil erosion on the hillslope system changed vegetation condition by wildfire The rainfall energy, input energy consisted of kinetic and potential energy, is influenced by vegetation coverage and height. Output energy at the outlet of hillslope is decided as the kinetic energy of runoff and erosion soil, and mechanical work according to moving water and soil is influenced dominantly by the work rather than the kinetic energy. Relationship between output and input energy is possible to calculate the energy loss in the runoff and erosion process. The absolute value of the energy loss is controlled by the input energy size of rainfall because energy losses of runoff increase as many rainfall pass through the hillslope system. The energy coefficient which is dimensionless is defined as the ratio of input energy of rainfall to output energy of runoff water and erosion soil such as runoff coefficient. The energy coefficient and runoff coefficient showed the highest correlation coefficient with the vegetation coverage. Maximum energy coefficient is about 0.5 in the hillslope system. The energy theory for output energy of runoff and soil erosion is presented by the energy coefficient theory associated with vegetation factor. Also runoff and erosion soil resulting output energy have the relation of power function and the rates of these increase with rainfall.

• The Korean Journal of Ecology
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• v.4 no.1_2
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• pp.1-7
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• 1981

Montane grassland at the summit of Mt. Soback, Korea, was studied to verify the relationships between environmental factors and vegetations on the different slopes. The contents of total nitrogen and excangeable cation and thickness of A-layer of soil in the east slope were greater and thicker than those of the northwest one. Two different community types were observed one, on the east slope, was a grass community and the other, on the northwest, was a grass community. Plant height and annual production of the forb community were taller and greater than those of the grass community. These differences might be correlated with the different of snow depth between two slopes caused by wind in witner. It is clear that the formation of the montane grassland at the study area is mainly caused by fire, wind and topography at the summit.

• Journal of The Korean Society of Grassland and Forage Science
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• v.9 no.1
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• pp.43-47
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• 1989

草地生態系에 있어서의 칼리 (K)의 動態에 관한 硏究의 한 부분으로서, 草地土壞의 表面에 놓인 牧 草落葉의 分解에 따른 칼리의 溶出狀況을 그외의 無機養分의 溶出과 比較하여, 칼리溶出의 特性을 알아 낼 目的으로 실험을 수행했다. 초지토양의 표면에 놓인 牧草葉은 1年의 시험기간중에 當初乾物量의 약30%로 分解되었으며, 그分解速度는 月隣水量보다는 平均氣溫과 더 높은 相關關係를 보였다. 낙엽분해에 따르는 植物體로 부터의 養分溶出은 칼리>인(P)>마그네슘(Mg), 질소(N)>칼슘(Ca)의 順l이었다. 칼리와 인은 1個月 경과후에 當初含有量의 40%와 45%로 현저하게 減少되었으며, 칼리는 그 以後에도 牧草의 分解에 따라 계속해서 溶出되어 9個月 째에는 1%로 減少되었다. 마그네슘과 질소는 목초의 분해와 거의 一致해서 溶出되었으나, 칼슘은 낙엽의 분해가 진행되어도 當初含有量에서 큰 減少가 일어나지 않았다. 以上의 結果로 부터 질소를 포함한 無機物의 溶出은 牧草의 分解와 대체로 같은 傾向을 나타내는 것을 알았으며, 칼리의 溶出은 특히 牧草落葉의 分解初期에 많다는 것을 알았다. 따라서 牧草落葉으로부터의 칼리의 溶出이 草地生態系에 있어서의 칼리의 再循環에 큰 役割을 하는 것으로 생각되어 졌다.