• 상하수도학회지
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• 제35권6호
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• pp.497-505
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• 2021

This paper investigates the current status of Jeju special self-governing province (JSSGP)'s water infrastructure and recommends directions for improvement. JSSGP relies on groundwater for most of its water resources. Recently, water usage has been steadily increasing due to the increase of residents and tourists while the quality of groundwater has been steadily worsening. Deterioration in water quality of groundwater can be seen through the increase in concentration of nitrate nitrogen and microorganisms. To overcome such problems, water consumption must be reduced by water demand management in all fields including residential and agricultural water use. The quality of water resources should be preserved through the management of pollutants. For efficient management of water resources, great efforts should be made to reduce the leakage rates in household and agricultural water, which is currently at the highest level in the country. Furthermore, diversification of water intake sources other than groundwater is needed, especially for agricultural water supply. For water and sewerage facilities, compliance with drinking water quality standards and discharge water quality standards must be achieved through the optimization of operation management. This process requires recruiting professionals, improving existing workers' expertise, and improving facilities.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 창립총회 및 춘계학술발표회
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• pp.24-27
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• 2000

The development of land classification and soil productivity rating systems (SPR) are examined for their application to valuation of agricultural land in South Dakota, USA. The application of SPR data to land valuation work conducted by real estate appraisers, tax assessors, and economists are discussed along with an assessment of its benefits and limitations.

• 지질공학
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• 제10권1호
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• pp.39-50
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• 2000

강원도 지역은 산악이 많아 농업용수의 개발이 시급하며 연구대상 지역인 춘천시 신북지역은 소양댐 하부지역에 위치하면서 댐의 혜택을 보지 못하고 벼농사를 하고 있다. 특히 고랭지 야채를 개발하고 높은 수익을 올리기 위해서는 지하수와 연관된 지열을 개발하여 추운 겨울에도 보온을 할 수 있는 시스템을 개발하여야 한다. 국내의 지하수는 1960년대부터 농업용수를 위하여 연구되었고 최근에는 지하철, 원자력 발전소와 같은 지하구조물이나 핵폐기물, 유류 지하저장장소와 같은 대단위 지하공사에서도 재해 방지를 위한 지하수맥의 정확한 조사가 요구되고 있다. 본 연구에서는 지하수 탐사를 위하여 전기탐사, 탄성파탐사, 지오레이더 탐사 등 복합탐사법을 적용하였다.

• 한국관개배수논문집
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• 제7권2호
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• pp.57-65
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• 2000

The effect of land use of an alluvial watershed in the upper North Han river basin on groundwater quality were investigated. Existing 20 farm wells were selected as monitoring wells representing different land uses of residential, arable(paddy and field),

• 한국농공학회논문집
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• 제52권3호
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• pp.65-71
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• 2010

This study was conducted to investigate the dynamics of nutrients such as total nitrogen (TN), nitrate nitrogen ($NO_3$-N) total phosphorous (TP), and phosphate phosphorous ($PO_4$-P) in outflow from a cabbage farmland in a mixed land-use watershed. The TN concentrations in groundwater showed twice peaks in late July 2006 and late March 2007 (3.8, 4.7 mg/L, respectively), when it rained shortly after fertilizer application, indicating that nitrogen leaching is greatly influenced by fertilization and rainfall. The mean concentrations of TN and $NO_3$-N in surface water were not significantly higher than those in groundwater, while the mean concentrations of TP and $PO_4$-P in surface water were significantly (p < 0.05) were higher than those in groundwater. The TN concentrations in groundwater were generally higher than those in surface water during fertilization and early growing season due to the effect of fertilization, but vice versa in the other periods. In contrast, the TP concentrations in groundwater were always lower than those in surface water due to the sorption of particulate phosphorous by soil. The ratio of TN load in baseflow to that in total TN load (39 %) was much greater than the TP ratio (7 %), suggesting that baseflow contribute to nitrogen export. Therefore, proper fertilization management should be taken to reduce nitrogen load through baseflow.

• 한국농공학회논문집
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• 제53권6호
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• pp.67-74
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• 2011

The objective of this study was to compare concentrations of nutrients such as total nitrogen (TN), nitrate nitrogen ($NO_3$-N) total phosphorous (TP), and phosphate phosphorous ($PO_4$-P) in groundwater under paddy and upland fields, and surface water recharging from a rural mixed land-use watershed. Chinese cabbage and hot pepper were cultivated on the upland field plot. The TN concentrations in upland groundwater showed double peaks (4.7, 4.3 mg/L, respectively) in April 2009 shortly after fertilizer application, indicating that TN concentrations are greatly influenced by fertilization. However, the TN concentrations in paddy groundwater were always lower than 2.0 mg/L irrespective of fertilization. Whereas the mean concentrations of TN and $NO_3$-N in upland groundwater significantly (p<0.05) higher than those in surface water, the mean concentrations of TP and $PO_4$-P in upland groundwater were significantly lower than those in surface water. On the other hand, the mean concentrations of TN, $NO_3$-N, TP and $PO_4$-P in paddy groudwater were significantly (p<0.05) lower than those in surface water. The TN concentrations in upland groundwater were generally higher than those in surface water during early April to early December due to the effect of fertilization, but vice versa in the other periods. In contrast, the TP concentrations in upland groundwater were always lower than those in surface water due to the sorption of inorganic phosphorous by soil. Moreover, the TN and TP concentrations in paddy groundwater were always lower than those in surface water, and therefore paddy groundwater may dilute nutrient concentrations in surface water when paddy groundwater and surface water mix.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2007년도 학술발표회 논문집
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• pp.8-14
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• 2007

Water quality in Lake Rotorua, New Zealand, deteriorated since the 1960s because of excessive phytoplankton growths due principally to increasing nitrogen and phosphorus in the lake waters. Nutrient concentrations in eight of the nine major streams feeding Lake Rotorua have increased since 1965. The groundwater system has a key role in the hydrology of the Lake Rotorua catchment and the groundwater system is probably the control on the time delay between intensification of agricultural land use and response of surface water quality. All major, and many minor streams, in the catchment are fed by springs. Two lithological units are most important to groundwater flow in the Lake Rotorua catchment: Mamaku Ignimbrite, erupted in about 200,000 years ago and Huka Formation sediments which filled the caldera left by the Mamaku Ignimbrite eruption. Rainfall recharge to groundwater in the groundwater catchment of Lake Rotorua is estimated as approximately 17300 L/s. A calibrated steady-state groundwater flow model estimates that approximately 11100 L/s of this flow discharges into streams and then into the lake and the balance travels directly to Lake Rotorua as groundwater discharge through the lake bed. Land use has impacted on groundwater quality. Median Total Nitrogen (TN) values for shallow groundwater sites are highest for the dairy land use (5.965 mg/L). Median TN values are also relatively high for shallow sites with urban-road and cropping land uses (4.710 and 3.620 mg/L, respectively). Median TN values for all other uses are in the 1.4 to 1.5 mg/L range. Policy development for Lake Rotorua includes defining regional policies on water and land management and setting an action plan for Lake Rotorua restoration. Aims in the action plan include: definition of the current nutrient budget for Lake Rotorua, identification of nutrient reduction targets and identification of actions to achieve targets. Current actions to restore Lake Rotorua water quality include: treatment of Tikitere geothermal nitrogen inputs to Lake Rotorua, upgrade of Rotorua City sewage plant, new sewage reticulation and alum dosing in selected streams to remove phosphorus.

• 터널과지하공간
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• 제27권4호
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• pp.205-216
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• 2017

지하수위 변동은 석회석 폐광산에서 발생하는 지반침하의 주된 요인이다. 본 연구에서는 지하수로 포화된 석회석 채굴공동에서 발생하는 지하수 유동을 자연상태와 골재 충전, 임시배수로 구분하여 지반 안정성에 미칠 영향을 3차원 지하수 유동 해석을 통해 평가하였다. 해석 결과 골재 충전시 지반 및 소류지의 지하수위가 상승하였지만 강우나 소류지 농업용수 사용으로 발생하는 수위차 보다 작고 유속 또한 자연상태의 유속과 유사하게 나타났다. 임시배수시에는 지반 및 소류지의 지하수위가 급격하게 하강하고 공동 내 유속이 최대 25배 이상 증가하는 것으로 나타나 지반침하 위험성이 증가하는 것으로 나타났다.

• 한국농공학회논문집
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• 제64권2호
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• pp.27-35
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• 2022

Based on the current status of groundwater usage in the dry season through field surveys, this study tried to suggest countermeasures to reduce groundwater usage and to improve the water quality of baseflow from agricultural fields. For this purposes, basins with water curtain cultivation preceded were targeted where decreases of groundwater due to continuous use of groundwater in spring and winter annually observed. From monitoring groudwater usage of the study watershed, 130,058, 130,105 m³/day of water was pumped in during the water curtain cultivation period (October-February) in the Shindun, Seokwon watershed respectively. And the pilot application of the smart automated sensor-based water curtain cultivation system (smart WC system) developed in this study to reduce groundwater consumption has been conducted. As a result, the efficiency of the smart WC system when threshold temperature is set as 6.3 ℃ was 21.1% compared to conventional cultivation and efficiency increased as threshold temperature gets lower. Lastly, in this study, culvert drainage and Bio-filters were installed and rainfall monitoring was performed 15 times in order to analyze the baseflow securement and pollutant loads behavior. As a result, the test-bed with culvert drainage and Bio-filter installed together generated 61.4% more baseflow (4.974 m³) than the test-bed with only culvert drainage was installed (3.056 m³). However, the total pollutant load of all water quality contents (BOD, COD, T-N, TOC) except for the SS and T-P was found to be greater in the culvert drain and Bio-filter installed than in the culvert drain test-bed.

• 한국수자원학회논문집
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• 제35권1호
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• pp.97-108
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• 2002

도시화가 빠르게 진행된 부천시 지역의 수질조사 당시 토지이용을 토지이용 변화과정에 의해 세부 분류하고 토지이용과 토지이용기간에 따른 지하수 수질차이 여부를 비모수통계기법으로 검정하였다. 연구지역에서 검출빈도가 높은 7개 성분의 수질자료를 이용하였다. 수질조사 당시 토지이용이 동일한 지역에서 천부지하수 수질은 토지이용기간에 따라 통계적으로 유의한 차이를 보인다. 20년 이상 이용된 오래된 주거지역의 과망간칼륨소비량(이하 KMnO$_4$), 경도 등의 농도는 10년 정도 이용된 새로운 주거지역보다 통계적으로 유의한 정도로 높은 경향을 보인다. 천부지하수 수질은 토지이용기간이 유사한 지역에서 토지이용에 따라 유의한 차이를 보인다. 주거지역은 농경지(2~5년 전까지 논으로 이용된 지역)에 비해 NO$_3$-N, 경도, 증발잔류물의 농도가 유의하게 높고 중위수는 2.2~3.8배 크게 나타난다. 공업지역은 농경지에 비해 NO$_3$-N, KMnO$_4$, Cl$^{-}$ 이온의 농도가 유의하게 높고, 중위수는 5.5~18배 정도 크며, 주거지역에 비해 KMnO$_4$의 농도가 유의하게 높고 중위수는 12배 정도 크게 나타난다. 도시화가 빠르게 진행된 지역에서 천부지하수 수질의 공간분포는 토지이용과 함께 이용기간과 관계가 있으며, 이것은 손상된 하수관에서 지하수로 유입되는 오염물질 농도와 하수관의 누수율 차이에 기인한 것으로 판단된다.로 판단된다.