• 제목/요약/키워드: Water conductivity

검색결과 1,911건 처리시간 0.027초

수목(樹木)의 수분특성(水分特性)에 관한 생리(生理)·생태학적(生態學的) 해석(解析(III) - 몇 종(種)의 침엽수(針葉樹)에 있어서 Shoot Water Potential의 일변화(日變化) 및 Xylem Conductivity의 특성(特性) - (Ecophysiological Interpretations on the Water Relations Parameters of Trees(III) - Diurnal Change of Shoot Water Potential and Characteristics of Xylem Conductivity in Several Conifers -)

  • 한상섭;전두식
    • 한국산림과학회지
    • /
    • 제63권1호
    • /
    • pp.21-27
    • /
    • 1984
  • 본(本) 연구(硏究)는 몇 종(種)의 침엽수(針葉樹)에 대하여 Shoot water potential의 일변화(日變化) 및 지(枝)의 Xylem conductivity의 특성(特性)을 측정고찰(測定考察)한 것으로 다음과 같은 결과를 얻었다. 1) Shoot water potential은 광도(光度)의 크기에 따라 변화(變化)하며, 광도(光度)의 감소(減少)가 시작된지 2시간(時間) 늦게 Shoot water potential의 증가(增加)가 시작되었다. 2) 지엽(枝葉)의 일중(日中) 최대수분(最大水分) 결차(缺差)는 12시(時)부터 14시(時) 사이에 일어나며, 그 값의 크기는 일본잎갈나무 -22 bar, 잣나무 -18 bar, 소나무 -15 bar, 젓나무 -14 bar, 리기다소나무 -10 bar 정도였다. 3) 수고(樹高) 1 m 당(當) 지엽(枝葉)의 수분결차(水分缺差)의 크기를 경사도(傾斜度)(${\varphi}_L/m$)로 나타내면 잣나무 -1.7 bar/m, 일본잎갈나무 -2.1 bar/m였다. 4) 지(枝)의 Relative Xylem conductivity (K, $cm^2/hr{\cdot}atm$)의 평균치(平均値)는 일본잎갈나무 2878, 리기다소나무 2763, 소나무 2652, 잣나무 2113 이었다.

  • PDF

토양 열전도를 이용한 토양함수비 예측에 관한 연구 (A Study for Prediction of Water Contents in Soil by Using the Soil Thermal Conductivity)

  • 조진우;강도경;강이석
    • 한국군사과학기술학회지
    • /
    • 제18권2호
    • /
    • pp.125-130
    • /
    • 2015
  • Vehicles and UGV(Unmanned Ground Vehicle) need a variety of road informations, such as road profile, soil type and soil water contents, to run a cross country course. Especially, soil water contents are very important factor to judge the vehicle mobility, because it can change soil strength. This paper describes the real-time measuring method of soil water contents by using the soil thermal conductivity.

플로우 펌프기법을 이용한 포천지역 화강 풍화토의 함수특성곡선 (Soil-Water Characteristic Curve of Weathered Granite Soils in Pocheon Area using Flow Pump Technique)

  • 이강일;이준용;백원진
    • 한국농공학회논문집
    • /
    • 제51권1호
    • /
    • pp.11-20
    • /
    • 2009
  • Flow pump technique was used in order to determine the soil-water characteristic curve of weathered granite soils in Pocheon area. This technique enables measurement to be more convenient and accurate as it is based on the CU condition of triaxial compression test. Besides, it is also able to measure dry and moisture curves continuously since the test is controled by means of a computer automatically. In this study, not only a hydraulic conductivity of weathered granite soils at fully saturated state in Pocheon area, but also a soil-water characteristic curve throughout unsaturate flow tests were determined. In addition, Brooks and Corey's model and Genuchten's model were used to simulate the soil-water characteristic curve. On the basis of the simulation an unsaturate hydraulic conductivity was predicted.

남극 및 시베리아 흙의 동토공학적 특성 분석 (Engineering Characteristics of Antarctic and Siberian Frozen Soils)

  • 김영진;신재원;김현기
    • 한국지반공학회:학술대회논문집
    • /
    • 한국지반공학회 2008년도 춘계 학술발표회 초청강연 및 논문집
    • /
    • pp.894-904
    • /
    • 2008
  • In this study, soil samples from the Antarctic and Vladivostok, Siberia were tested in the laboratory, and specific gravity, compaction curve and grain size distribution were determined. The effect of temperature change on the thermal conductivity, unfrozen water content and compressive strength were investigated. Samples for the compressive strength test were prepared in a mold with a fixed volume to prevent swelling and the effect of temperature and water content change on the strength were compared. Results from the thermal conductivity test showed that thermal conductivity values for both soils were larger at temperatures below freezing than above freezing. The unfrozen water content dropped sharply within a temperature range of $0{\sim}-5^{\circ}C$ and then gradually decreased further up to $-20^{\circ}C$. Compressive strength test results showed various stress/deformation curves with a change in water content. Sandy soil had much larger strength than pure ice at an identical temperature, while clayey soil had a smaller strength than ice near the freezing point, but showed a larger strength at temperatures belows $-15^{\circ}C$.

  • PDF

MgO.$P_2O_5$ 유리의 전기전도도에 미치는 수분의 영향 (Effects of Water on the Electrical Conductivity of Magnesium Metaphosphate Glasses)

  • 강은태;박용완
    • 한국세라믹학회지
    • /
    • 제23권4호
    • /
    • pp.85-89
    • /
    • 1986
  • Electrical conductivity have been measured as function of temperature in MgO.$P_2O_5$ glasses containing small amounts of water. Conduction was due to the contribution of $H^+$ and the mobility of protons in the glass increased linearly with increasing its concentration. The conductivity was pro-portional to the square of the proton concentration and the activation energy decreased linerly with increasing logarithm of the proton concentration, And $$\sigma$_0$ and $A_0$ was independent of the proton concentration but not on glass compositions.

  • PDF

폐비닐 골재 혼합토의 기본 성질에 관한 연구 (A Fundamental Study on the Waste Polyethylene Chips Mixed with Soil)

  • 김영진;김현민
    • 한국지반공학회:학술대회논문집
    • /
    • 한국지반공학회 2000년도 봄 학술발표회 논문집
    • /
    • pp.548-555
    • /
    • 2000
  • It was investigated whether the waste polyethylene chips can be recycled as construction materials in geotechnical engineering field. The standard Proctor test, the hydraulic conductivity test, the large box direct shear test, the thermal conductivity test, the frost heaving test and the time domain reflectometry test were performed on weathered granite soil mixed with variable amount of the waste polyethylene chips. The experimental results showed that the hydraulic conductivity and the shear strength of weathered granite soil increase with increasing the amount of the waste polyethylene chips. On the other hand, the thermal conductivity, the amount of frost heaving and the unfrozen water contents of weathered granite soil decrease with increasing the amount of the waste polyethylene chips.

  • PDF

튜브의 열전도도와 튜브 외면에서의 대류열전달이 보텍스튜브의 에너지 분리에 미치는 영향 (The Effect of the Thermal Conductivity of a Tube and the Convective Heat Transfer on the Outer Surface of a Tube on the Energy Separation in Vortex Tubes)

  • 유갑중;이병화;최병철
    • 설비공학논문집
    • /
    • 제13권9호
    • /
    • pp.845-852
    • /
    • 2001
  • The phenomena of energy separation in vortex tubes was investigated experimentally to see the effects of the conductivity of a tube and convective heat transfer on the outer surface of a tube. The experiment was carried out with different conductivity (pyrex, stainless steel and copper) of a tube and three kinds of convective heat transfer modes (adiabatic condition, natural convection (air) and forced convection (water) on the outer surface of a tube. the results were obtained that hot exit fluid temperature was highly affected by a change of conductivity of a tube when the outer surface was cooled by the forced convection of water. However, the cold exit temperature was little affected by heat transfer modes on the outer surface in vortex tubes.

  • PDF

Determination of trace bromate in various water samples by direct-injection ion chromatography and UV/Visible detection using post-column reaction with triiodide

  • Kim, Jungrae;Sul, Hyewon;Song, Jung-Min;Kim, Geon-Yoon;Kang, Chang-Hee
    • 분석과학
    • /
    • 제33권1호
    • /
    • pp.42-48
    • /
    • 2020
  • Bromate is a disinfection by-product generated mainly from the oxidation of bromide during the ozonation and disinfection process in order to remove pathogenic microorganism of drinking water, and classified as a possible human carcinogen by International Agency for Research of Cancer (IARC) and World Health Organization (WHO). For the purpose of determining the trace level concentration of bromate, several sensitive techniques are applied mostly based on suppressed conductivity detection and UV/Visible detection after postcolumn reaction (PCR). In this study, the suppressed conductivity detection method and the PCR-UV/Visible detection method through the triiodide reaction were compared to analyze the trace bromate in water samples and estimated for the availability of these analytical methods. In addtion, the state-of-the-art techniques was applied for the determination of trace level bromate in various water matrices, i.e., soft drinking water, hard drinking water, mineral water, swimming pool water, and raw water. In comparison of two analytical methods, it was found that the conductivity detection had the suitable advantage to simultaneously analyze bromate and inorganic anions, however, the bromate might not be precisely quantified due to the matrix effect especially by chloride ion. On the other hand, the trace bromate was analyzed effectively by the method of PCR-UV/Visible detection through triiodide reaction to satisfactorily minimize the matrix interference of chloride ion in various water samples, showing the good linearity and reproducibility. Furthermore, the method detection limit (MDL) and recovery were 0.161 ㎍/L and 101.0-108.1 %, respectively, with a better availability compared to conductivity detection.

북한산국립공원의 계류수질 보전 전략 (II) ­-계류수질오염 영향인자를 중심으로­- (Conservation Strategy on Stream Water Quality in the Mt. Bughansan National Park (II) -­With a Special Reference to the Factor influenced on Stream Water Quality Pollution­-)

  • 박재현
    • 한국환경복원기술학회지
    • /
    • 제5권1호
    • /
    • pp.8-18
    • /
    • 2002
  • This research was conducted to establish the conservation strategy of stream water quality by analyzing the factors influenced on stream water quality in the northeastern part of Mt. Bughansan National Park from July 1998 to October 2001. The number of visitors resulted in the significant increase of electrical conductivity, which affected on pollution of the stream water quality. According to the multiple regression analysis, the pH of the stream water was related to dissolved oxygen and temperature of water at the 1% significant level. The electrical conductivity of the stream water was related to number of visitors, amount of $K^+$ and ${NO_3}^-$, total amount of ions, percentages of $Cl^-$ and $Na^+$ caused by solifluction soil at the 1% significant level. The anions($Cl^-$, ${NO_3}^-$ and ${SO_4}^{2-}$) of the stream water were related to number of visitors, electrical conductivity, air temperature, hardness, amount of ${NO_3}^-$, ${SO_4}^{2-}$, total ions, percentage of $Cl^-$, ${NO_3}^-$, ${SO_4}^{2-}$, amount of $Ca^{2+}$ caused by solifluction soil at the 1% significant level. To prevent the pollution of stream water in the northeastern part of Mt. Bughansan National Park, it is recommended that the number of visitors in the park should be managed and rehabilitated rapidly by measure to eco-friendly during the spring season.

수두손실률, 투수계수 및 공극비의 상호관계를 통한 제체의 다짐상태 평가 (The Estimation of Compacted State on Sea Dike Embankment with the Interrelationships Between the Hydraulic Head Loss Rate, the Hydraulic Conductivity and the Void Ratio)

  • 임성훈
    • 한국농공학회논문집
    • /
    • 제57권1호
    • /
    • pp.11-23
    • /
    • 2015
  • In this study the laboratory test for hydraulic conductivity and the seepage analysis with finite element method on measurement section of sea dike embankment were performed for the purpose of estimating the relative density of embankment from the measured pore water pressures, and both results of the test and the analysis were coupled with the method of estimating seepage blocking state with the hydraulic head loss rate in sea dike embankment. The relationship of void ratio vs hydraulic head loss rate was obtained by setting hydraulic conductivity as common ordinate on the relationships between the void ratio and the hydraulic conductivity and between the hydraulic conductivity and the hydraulic head loss rate. The void ratio on the segment between measuring points was calculated from the coupled relationship of the void ratio vs the hydraulic conductivity. The allowable upper and lower limits of hydraulic head loss rate and those of void ratio on the safety were generated from the coupled relationship between the laboratory compaction test and the sedimentation test. Current hydraulic head loss rate and void ratio were evaluated in the allowable range between upper and lower limits.