• 한국지형학회지
• /
• 제23권1호
• /
• pp.77-85
• /
• 2016

To understand the difference of runoff discharge processes between Gwangneung deciduous and coniferous forest catchments, we collected hydrological data (e.g., precipitation, soil moisture, runoff discharge) and conducted hydrochemical analyses in the deciduous and coniferous forest catchments in Gwangneung National Arboretum in the northwest part of South Korea. Based on the end-member mixing analysis of the three storm events during the summer monsoon in 2005, the hillslope runoff in the deciduous forest catchment was higher 20% than the coniferousforest catchment during the firststorm event. Howerver, hillslope runoff increased from the second storm event in the coniferous catchment. We conclude that low soil water contents and topographical gradient characteristics highly influence runoff in the coniferous forest catchment during the first storm events. In general, coniferous forests are shown high interception loss and low soil moisture compared to the deciduous forests. It may also be more likely to be a reduction in soil porosity development when artificial coniferous forests reduced soil biodiversity. The forest soil porosity is an important indicator to determine the water recharge of the forest. Therefore, in order to secure the water resources, it should be managed coniferous forests for improving soil biodiversity and porosity.

• 한국산림과학회지
• /
• 제99권5호
• /
• pp.755-761
• /
• 2010

This study analyzed water quality data from a coniferous forest catchment in order to quantify the contributions of runoff components to stormflow, and to understand the effects of antecedent moisture conditions within catchment on the contributions of runoff components. Hydrograph separation by the twocomponent mixing model analysis was used to partition stormflow discharge into pre-event and event components for total 10 events in 2005 and 2008. To simplify the analysis, this study used single geochemical tracer with Na+. The result shows that the average contributions of event water and pre-event water were 34.8% and 65.2% of total stormflow of all 10 events, respectively. The event water contributions for each event varied from 18.8% to 47.9%. As the results of correlation analysis between event water contributions versus some storm event characteristics, 10 day antecedent rainfall and 1 day antecedent streamflow are significantly correlated with event water contributions. These results can provide insight which will contribute to understand the importance of antecedent moisture conditions in the generation of event water, and be used basic information to stormflow generation process in forest catchment.

• 한국농림기상학회지
• /
• 제13권4호
• /
• pp.157-164
• /
• 2011

침엽수인공림에서 임분 성장 및 간벌이 장기 물수지에 미치는 영향을 파악하기 위하여 광릉 침엽수인공림유역 및 활엽수천연림유역에서 1982년부터 2009년까지 28년에 걸쳐 관측한 연강수량 및 연유출량의 변화를 분석하였다. 광릉 침엽수인공림유역은 1976년에 유역 전반에 걸쳐 잣나무와 전나무, 리기다소나무가 3,000본/ha의 밀도로 식재되었으며, 1996년에 잔존 본수의 약 45%를 간벌하였다. 1982년부터 2009년까지의 기간을 광릉 침엽수인공림유역 내 침엽수림의 영급을 기준으로 4개 기간으로 구분하여 연평균 강수량 및 유출량을 비교한 결과, 활엽수천연림유역의 기간별 연평균 유출량은 강수량이 증가함에 따라 동일하게 증가하는 추세를 보였으나, 침엽수인공림유역에서는 임령증가 및 간벌 실시에 따라 증감을 반복하는 것으로 나타났다. 간벌을 실시하지 않은 침엽수인공림은 임령이 증가할수록 높은 식재밀도로 인해 수관울폐도가 과도하게 높아지고 이로 인해 수관차단 및 증산량 증가 등 물손실이 커진다. 본 연구에서도 간벌 실시전 침엽수인공림유역의 연평균 유출량이 감소하였으나 간벌 실시 후에는 간벌 전에 비해 연평균 유출량이 약 1.7배 증가하는 등 유출량 증가 경향이 뚜렷하였다. 이러한 경향은 연강수량 및 연유출량의 이중 누가곡선 비교분석에서도 동일하게 나타났다. 본 연구에서는 간벌 후 약 10년 경과시 연강수량의 뚜렷한 증가 경향에도 불구하고 침엽수인공림유역의 유출량이 다시 감소하였는데, 이는 임분이 성장함에 따라 수관차단 등 물손실량이 다시 증가하기 때문이다. 따라서, 침엽수인공림유역에서 지속적인 수자원 확보를 위해서는 10년 이내의 간격으로 적정한 밀도의 간벌을 반복해서 실시하는 것이 바람직할 것으로 판단된다.

• 한국산림과학회지
• /
• 제95권5호
• /
• pp.556-561
• /
• 2006

This study was conducted to choose end-members and tracers for application of End Member Mixing Analysis (EMMA) model for the coniferous forest catchment, Gwangneung Gyeongi-do near Seoul metropolitan of South Korea (N $37^{\circ}$ 45', E $127^{\circ}$ 09'). This coniferous forest of Pinus Korainensis and Abies holophylla was planted at stocking rate of $3.0stems\;ha^{-1}$ in 1976. Thinning and pruning were carried out two times in the spring of 1996 and 2004 respectively. We monitored two successive rainfall events during ten days from June 26, 205 to July 5, 2005. Two storm events were selected to determine the end members and natural traces for hydrograph separation. The event 1 amounts to 161.9 m for two days from June 26 to 27, 2005. The event 2 precipitates to 139.2 mm for one day of July 1, 205. Throughfall, groundwater, soil water and stream water of the two events above were sampled through the bulk and automatic sampler. Their chemical properties were analyzed for prediction of the main tracer. The end members that contribute to the stream runoff were identified from the three components including groundwater, soil water and throughfall. Each component and stream water in the two events formed the suitable mixing diagram in case of chloride-nitrate ion and sulfate-potassium ion. Especially, chloride-nitrate ion was found to be the most suitable tracers for EMMA model in the two events.

• 한국산림과학회지
• /
• 제96권5호
• /
• pp.561-566
• /
• 2007

This study was conducted to clarify runoff production processes in forested catchment through hydrograph separation using three-component mixing model based on the End Member Mixing Analysis (EMMA) model. The study area is located in the coniferous-forested experimental catchment, Gwangneung Gyeonggido near Seoul, Korea (N 37 45', E 127 09'). This catchment is covered by Pinus Korainensis and Abies holophylla planted at stocking rate of 3,000 trees $ha^{-1}$ in 1976. Thinning and pruning were carried out two times in the spring of 1996 and 2004 respectively. We monitored 8 successive events during the periods from June 15 to September 15, 2005. Throughfall, soil water and groundwater were sampled by the bulk sampler. Stream water was sampled every 2-hour through ISCO automatic sampler for 48 hours. The geochemical tracers were determined in the result of principal components analysis. The concentrations of $SO_4{^{2-}$ and $Na^+$ for stream water almost were distributed within the bivariate plot of the end members; throughfall, soil water and groundwater. Average contributions of throughfall, soil water and groundwater on producing stream flow for 8 events were 17%, 25% and 58% respectively. The amount of antecedent precipitation (AAP) plays an important role in determining which end members prevail during the event. It was found that ground water contributed more to produce storm runoff in the event of a small AAP compared with the event of a large AAP. On the other hand, rain water showed opposite tendency to ground water. Rain water in storm runoff may be produced by saturation overland flow occurring in the areas where soil moisture content is near saturation. AAP controls the producing mechanism for storm runoff whether surface or subsurface flow prevails.

• 한국농림기상학회지
• /
• 제7권1호
• /
• pp.51-56
• /
• 2005

To understand the chemical changes in the streamwater and contribution of subsurface discharge during the storm event, we analyzed electric conductivity (EC), anions, and cations in Gwangneung deciduous and coniferous forest catchment. The stream water samples were collected three times in 2004 by using an auto-sampler: September 7-9 (E040907-D and -C; where D and C indicate deciduous and coniferous forest catchment, respectively), September 11-13 (E040911-D and -C), and September 16-18 (E040916-D and -C). We found a negative relationship between discharge intensity and EC in streamwater. The E040911 and E040916 showed slack change of stream discharge in comparison to E040907 due to contribution of base flow recharged by much precipitation. Moreover, NO/sub 3//sup -/ concentrations in E040911-C were highest, which may have resulted from forest management such as thinning in 2004. The relationship between pH and alkalinity in stream water showed that much of stream water have been recharged through subsurface. We conclude that subsurface discharge highly influences streamwater quality in a forested catchment, and the seperation of stream water discharge is therefore necessary to sustainable water management.

• 한국산림과학회지
• /
• 제90권2호
• /
• pp.197-209
• /
• 2001

준분포형 수문모형인 TOPMODEL은 산림유역의 유출량, 주 유출경로 및 수질을 공간적으로 예측하는데 많이 적용된다. TOPMODEL은 물리모형이 아니라 일종의 개념모형이며 주요 구성요소는 지형지수와 토양의 수평전달계수로 각각 지표면과 지표하 유출의 기여면적을 계산하는데 이용된다. 본 연구는 우리나라의 소규모 산림유역에서 TOPMODEL의 적용성을 검증하기 위하여 수행되었다. 시험지는 1979년부터 임업연구원에서 운용하고 있으며 서울 근교 경기도 광릉시험림에 위치해 있다. 활엽수림 유역은 임령이 약 80년, 유역면적이 22.0ha이고, 침엽수림 유역은 임령이 약 22년, 유역면적이 13.6ha이다. 관측자료는 활엽수 유역의 경우 1995년 7월과 2000년 6월에 발생한 2개 강우-유출사상이고 침엽수 유역의 경우 1995년과 1999년 7월 그리고 2000년 8월의 3개 강우-유출사상을 이용하였다. 지형지수는 $10m{\times}10m$의 수치지형도를 만들어 계산하였다. 지형지수 분포는 활엽수림 유역의 경우 2.6에서 11.1, 침엽수림 유역은 2.7에서 16.0으로 나타났다. 모형의 예측 효율성을 목적함수로 최적화한 결과 모형매개변수(m)와 유역의 평균 포화수평전달계수($lnT_0$)가 높은 민감도를 나타내었다. 매개변수의 최적값은 활엽수림 유역의 경우 m값은 0.034와 0.038 그리고 $lnT_0$값은 8.672와 9.475였으며, 침엽수 유역의 경우 m값은 0.031, 0.032, 0.033 그리고 $lnT_0$값은 5.969, 7.129, 7.575였다 이들 값을 이용하여 모의한 결과 모형의 예측 효율성은 활엽수림 0.958과 0.909 그리고 침엽수림 0.825, 0.922와 0.961로서 비교적 높게 나타났다. 강우-유출량 관측치와 모의치를 이용하여 강우-수문곡선을 작성한 결과 두 유역 모두 유출지연시간은 잘 일치하였다. 일부 강우-유출사상의 경우 총유출량과 첨두유량의 관측치와 모의치 간에 다소 차이를 보였지만 TOPMODEL은 전반적으로 10% 이하의 오차범위에서 총유출량과 첨두유량을 예측할 수 있었다. 결론적으로 TOPMODEL은 우리나라의 미계측 산림유역에서 유출량을 산정하는데 유용한 수문모형이다.

• 한국환경복원기술학회지
• /
• 제9권4호
• /
• pp.52-59
• /
• 2006

This study was conducted to find end-members and tracers which are effective to be applied in the End Member Mixing Analysis (EMMA) model for runoff separation at the Gwangneung coniferous forest catchment (13.6ha), Gyeonggido, Korea. We monitored three successive rainfall events during two weeks from June 26, 2005 to July 10, 2005, and analysed chemical properties of rainfall, throughfall, stemflow, groundwater and soil water considered as main components of storm runoff. The followings are the results of analyses of each component and tracer. Groundwater, soil water and rainfall (or throughfall) were dominant runoff components. Rainfall and groundwater were selected as main components for the two components-one tracer mixing model, and groundwater, soilwater and throughfall were selected as main components for the three components-two tracers mixing model. Tracers were selected from anion ($Cl^-$ and ${SO_4}^{2-}$), cation ($Na^+$, $K^+$, $Mg^{2+}$, and $Ca^{2+}$) and Acid Neutralizing Capacity (ANC) in event 1, 2, and 3. $Na^+$, $Ca^{2+}$ and ANC were selected in the two components-one tracer mixing model and ${SO_4}^{2-}-K^+$, ${SO_4}^{2-}-Na^+$, ${SO_4}^{2-}-Ca^{2+}$, ${SO_4}^{2-}$-ANC, and $Ca^{2+}$-ANC were selected in the three components-two tracers mixing model. Selected main runoff components and tracers can provide basic information to determine the contribution rate of each runoff component and identify the runoff process in a forest watershed.

• 한국산림과학회지
• /
• 제96권5호
• /
• pp.591-601
• /
• 2007

Spatial information on forest biomass is an important factor to evaluate the capability of forest as a carbon sequestrator and is a core independent variable required to drive models which describe ecological processes such as carbon budget, hydrological budget, and energy flow. The objective of this study is to understand the relationship between satellite image and field data, and to quantitatively estimate and map the spatial distribution of forest biomass. Landsat Enhanced Thematic Mapper (ETM+) derived vegetation indices and field survey data were applied to estimate the biomass distribution of mountainous forest located in Gwangneung Experimental Forest (230 ha). Field survey data collected from the ground plots were used as the dependent variable, forest biomass, while satellite image reflectance data (Band 1~5 and Band 7), Normalized Difference Vegetation Index (NDVI), Soil-Adjusted Vegetation Index (SAVI), and RVI (Ratio Vegetation Index) were used as the independent variables. The mean and total biomass of Gwangneung catchment area were estimated to be about 229.5 ton/ha and $52.8{\times}10^3$ tons respectively. Regression analysis revealed significant relationships between the measured biomass and Landsat derived variables in both of deciduous forest ($R^2=0.76$, P < 0.05) and coniferous forest ($R^2=0.75$, P < 0.05). However, there still exist many uncertainties in the estimation of forest ecosystem parameters based on vegetation remote sensing. Developing remote sensing techniques with adequate filed survey data over a long period are expected to increase the estimation accuracy of spatial information of the forest ecosystem.

• 한국농림기상학회지
• /
• 제8권3호
• /
• pp.174-182
• /
• 2006

이 연구는 임분구조가 다른 3가지 임상에서 장기 증발산량과 유출량의 변화를 분석하여 증발산량, 첨두유출량 및 유출량에 미치는 장기 임상변화의 효과를 밝히기 위하여 수행하였다. 시험지는 경기도 광릉에 소재한 국립산림과학원 유역수문시험지로서 인공침엽수 유령림과 천연활엽수 장령림 그리고 경기도 양주에 소재한 혼효 사방복구림을 대상으로 하였다. 수문자료는 1982년부터 1999년까지 양수댐에서 측정한 유출량과 강수량을 분석하여 각 시험지별로 약 110개의 홍수수 문곡선을 선별한 후 첨두유출량과 그 시점까지의 강수량 합계를 분석하였다. 강수량과 유출량의 관계로부터 증발산량을 추정한 결과, 증발산량은 인공침엽수 유령림에서 679mm, 천연활엽수 장령림에서 580mm이었으며 혼효 사방복구림에서는 368mm이었다. 또한, 유역의 유출량조절효과를 보여주는 유출량-지속기간 곡선에 대한 분석 결과, 임상이 가장 불량한 혼효 사방복구림에서 곡선의 기울기가 가장 급한 것으로 나타났으나, 산림이 생장함에 따라 그 기울기가 감소하는 것으로 분석되었다. 강수량과 첨두유출량의 관계를 분석한 결과, 인공침엽수 유령림과 혼효 사방복구림의 경우 각각 강수량 100mm 및 50mm에서 첨두유출량의 증가율이 높아지는 역치값을 보이는 반면에 천연활엽수 장령림은 200mm로 나타났다. 장기간에 걸친 홍수수 문곡선의 비교 결과, 인공침엽수 유령림에서는 10년이 경과한 후 첨두유출량이 감소한 것으로 나타나, 산림이 생장함에 따라 홍수유출조절 효과가 커지는 것으로 분석되었다.