• Title/Summary/Keyword: TDR Soil Moisture

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Spatial-temporal Distribution of Soil Moisture at Bumreunsa Hillslope of Sulmachun Watershed Through an Intensive Monitoring (설마천 유역 범륜사사면의 토양수분 시공간 집중변화양상의 측정)

  • Lee, Ga-Young;Kim, Ki-Hoon;Oh, Kyung-Joon;Kim, Sang-Hyun
    • Journal of Korea Water Resources Association
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    • v.38 no.5 s.154
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    • pp.345-354
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    • 2005
  • Time Domain Reflectometry (TDR) with multiplex system has been installed to configure the spatial and temporal characteristics of soil moisture at the Bumreunsa hillslope of Sulmachun Watershed. An intensive surveying was performed to build a refined digital elevation model (DEM) and flow determination algorithms with inverse surveying have been applied to establish an efficient soil moisture monitoring system. Soil moisture data were collected through intensive monitoring during 380 hrs in November of 2003. Soil moisture data shows corresponding variation characteristics of soil moisture on the upper, middle and lower parts of the hillslope which were classified from terrain analysis. Measured soil moisture data have been discussed on the context of physical process of hydrological modeling.

Movement Analyzing of Soil Moisture at a Hillslope Scale Considering Spatial-Temporal and Seasonal Characteristics (시공간적, 계절적 특성을 고려한 사면에서의 토양수분의 거동파악)

  • Oh, Kyung-Jun;Kwak, Yong-Seok;Do, Hoon-Kim;Kim, Sang-Hyun;Kim, Hyun-Jun;Kim, Nam-Won
    • Proceedings of the Korea Water Resources Association Conference
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    • 2006.05a
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    • pp.678-682
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    • 2006
  • In order to analyze movement of soil moisture, Time Domain Reflectometry(TDR) with multiplex system has been installed at the Bumreunsa hillslope of Sulmachun Watershed to configure spatial-temporal variation pattern considering seasonal characteristic. An intensive surveying was performed to build a refined digital elevation model(DEM) and flow determination algorithms with inverse surveying have been applied to establish an efficient soil moisture monitoring system. Soil moisture data were collected through an intensive and long term monitoring 380 hrs in November of 2003 and 1037 hrs in May and June of 2004. Soil moisture data shows corresponding variation characteristics of soil moisture on the up slope, buffer, main channel zones of the hillslope which were classified from terrain analysis. Inferences and limitations of measured soil moisture data were discussed in conjunction with flow characteristic through terrain analysis.

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Establishment and Operation of Soil Moisture Monitoring System Considering Temporal and Spatial Representation (시공간 대표성을 고려한 토양수분 모니터링 System의 구축 및 운영)

  • Kim, Ki Hoon;Kim, Sang Hyun;Lee, Ga Yeong;Kim, Won
    • Proceedings of the Korea Water Resources Association Conference
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    • 2004.05b
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    • pp.184-189
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    • 2004
  • A soil moisture measuring method for a hillslope of Korean watershed was developed to configure spatial-temporal distribution of soil moisture. Intensive surveying of topography had been performed to make a refined digital elevation model(DEM) and the hydrological interpretation from flow distribution algorithm was incorporated through reverse surveying. Moreover, A long term measurement system was established to maximize representative features of spatial variation of soil moisture and operated from October 19 to 21, 2003. TDR(Time Domain Reflectometry) with a multiplex monitoring system has been operated for accurate measurements. Measurements were performed at the right side hillslope of Buprunsa located at the sulmachun watershed. The data of temporal and spatial soil moisture variation by rainfall event were collected and the variations of soil moisture were well captured.

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Refractive index-based soil moisture sensor (굴절률 기반 토양 수분 센서)

  • Sim, Eun-Seon;Hwa, Su-Bin;Jang, Ik-Hoon;Na, Jun-Hee;Kim, Min-Hoi
    • Journal of Sensor Science and Technology
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    • v.30 no.6
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    • pp.415-419
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    • 2021
  • We developed a highly accurate, yet inexpensive, refractive index (RI)-based soil moisture sensor. To detect the RI, a light guide was set with a light-emitting diode and photodiode. When the air fills the space between the soil particles, most of the incident light is reflected at the interface between the waveguide and the air because of the large RI difference. As the moisture of the soil increases, the macroscopic soil RI increases. This allows incident light to pass through the interface. The intensity of the light reaching the photodiode was simulated according to the change in the soil RI. Using the simulation results, we designed and manufactured a curved glass waveguide. We evaluated the performance of the RI-based soil sensor by comparing it with a commercially available, high-cost and high-performance time-domain reflectometer (TDR). Our sensor was 96% accurate, surpassing the costly TDR sensor.

Soil Moisture Monitoring at a Hillslope Scale Considering Spatial-Temporal Characteristics (봄, 가을철 시공간적 특성을 고려한 사면에서의 토양수분 거동파악)

  • Oh Kyoung-Joon;Lee Hye-Sun;Kim Do-Hoon;Kim Hyun-Jun;Kim Nam-Won;Kim Sang-Hyun
    • Journal of Korea Water Resources Association
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    • v.39 no.7 s.168
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    • pp.605-615
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    • 2006
  • In order to analyze movement of soil moisture, Time Domain Reflectometry(TDR) with multiplex system has been installed at the Bumreunsa hillslope of Sulmachun Watershed to configure spatial-temporal variation pattern considering seasonal characteristic. An intensive surveying was performed to build a refined digital elevation model(DEM) and flow determination algorithms with inverse surveying have been applied to establish an efficient soil moisture monitoring system. Soil moisture data were collected through an intensive and long term monitoring 380 hrs in November of 2003 and 1037 hrs in May and June of 2004. Soil moisture data shows corresponding variation characteristics of soil moisture on the up slope, buffer, main channel zones of the hillslope which were classified from terrain analysis. Measured soil moisture data were discussed in conjunction with flow characteristic through terrain analysis. Regardless season, immediate responses of soil moisture about rainfall looks similar but recession and recharge are primary characteristics of intermediate soil moisture variation for spring to summer and fall to winter season, respectively.

Characterizing the Spatial-temporal Distribution of Soil Moisture for Sulmachun Watershed Through a Continuous Monitoring (설마천 유역의 토양수분 장기 모니터링을 통한 토양수분 시공간 변화양상의 특성화)

  • Lee, Ga Young;Kim, Ki Hoon;Kim, Sang Hyun
    • Proceedings of the Korea Water Resources Association Conference
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    • 2004.05b
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    • pp.209-214
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    • 2004
  • Time Domain Reflectometry with multiplex system has been installed to configure the spatial and temporal characteristics of soil moisture in a mountainous hillslope. An intensive surveying was performed to build a refined digital elevation model and flow determination algorithms with inverse surveying have been applied to establish an efficient soil monitoring system. Steady state wetness index, quasi-dynamic wetness index and fully dynamic wetness index have been calculated. Continuous monitoring of soil moisture data were analyized with wetness indices. Limitations and hydrological interpretations of this approach have beer discussed.

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Applicability of TDR Sensor for Monitoring Moisture Content of Landfill - Focusing on the 2nd Landfill of SUDOKWON Landfill Site - (매립지 함수율 모니터링을 위한 TDR 센서의 적용성 검토 - 수도권매립지 제2매립장을 중심으로 -)

  • Won-Young Choi;Young-Kyu Kim;Chul Hee Lee;Yong Jae Lee;Seung-Kyu Chun
    • Journal of Soil and Groundwater Environment
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    • v.29 no.4
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    • pp.1-11
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    • 2024
  • This study evaluated a method for prompt and periodic monitoring of moisture content in the waste layer of a landfill using a Time Domain Reflectometry (TDR) sensor, aimed at ensuring the stable operation of the bioreactor facility at the 2nd landfill of the SUDOKWON Landfill Site. It was found that the TDR sensor is sensitive to variables such as temperature changes and ion content in both the waste layer and leachate, indicating that a correction equation is necessary. A correction equation derived through regression analysis demonstrated a high correlation (correlation coefficient = 0.9647), and field verification experiments confirmed its reliability with an average deviation of only 1.5%. This verifies that the TDR sensor is effective for measuring and monitoring moisture content in landfills. It is also anticipated to be useful for various applications, including monitoring leachate levels, detecting leachate leakage, and assessing rainwater infiltration.

Establishment and Operation of a Soil Moisture Monitoring System Considering Temporal and Spatial Features of Representation (시공간 대표성을 고려한 토양수분 모니터링 System의 구축 및 운영)

  • Kim, Ki-Hoon;Kim, Sang-Hyun;Kim, Hyung-Sub;Kim, Won
    • Journal of Korea Water Resources Association
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    • v.38 no.1
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    • pp.73-82
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    • 2005
  • A soil moisture measuring method of a hillslope for Korean watershed is developed to configure spatial-temporal distribution of soil moisture. Intensive surveying of topography had been performed to make a digital elevation model(DEM). Flow distribution algorithms were applied and a distribution pattern of the measurement sensors was determined to maximize representative features of spatial variation of soil moisture. Inverse surveying provides appropriate information to install the waveguides in the field. Measurements were performed at the right side hillslope of Bumrunsa located at the Sulmachun watershed. A multiplex monitoring system has been established and spatial-temporal variation of soil moisture data has been measured for a rainfall-runoff event. Acquired soil moisture data show that physical hydrologic interpretations as well as the effectiveness of monitoring system. Lack of connectivity in vertical distribution of soil moisture suggests that preferential flow and macropore flux are important components in the hillslope hydrology.

Temperature Sensitivity Analysis of TDR Moisture Content Sensor for Road Pavement (도로하부 함수비 계측을 위한 TDR 방식 함수비 센서 온도 민감도 분석)

  • Cho, Myunghwan;Lee, Yoonhan;Kim, Nakseok;Jee, Keehwan
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.33 no.1
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    • pp.329-336
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    • 2013
  • The infrastructure of flexible pavement is composed of aggregate subbase, anti-frost layer, and subgrade. In particular, the subgrade performance is affected by climates such as frost action and precipitation. The method of TDR(Time Domain Reflectometry) sensors to measure moisture contents in subgrade layer has been used in the research. Due to the TDR method using dielectric permitivity of soil and water, the sensors can be affected by the low subgrade temperatures. The air temperatures frequently drops below $-20^{\circ}C$ in the winter in Korea. As a result, it is necessary to estimate the accuracy of the TDR moisture sensors in the range of below zero temperatures. In this study, the subgrade temperatures of lower than $-2^{\circ}C$ were extended to evaluate temperature sensitivity of the TDR moisture sensors. The test results revealed that the moisture contents around the sensors were reduced while those of the upper part of specimen showed a tendency to increase as the specimen surface temperature drops below zero under the volumetric moisture contents(VMC) of 20% and 30%. However, the impact of temperature on the function of the sensor at lower water contents was found to be negligible if any.

Development of Soil Moisture Monitoring System for Effective Soil Moisture Measurement for Hillslope Using Flow Distribution Algorithm and TDR (산지사면의 효과적인 토양수분 측정을 위한 흐름분배 알고리즘과 TDR을 이용한 토양수분 측정망의 구성)

  • Kang, Chang-Yong;Kim, Sang-Hyun;Jung, Sung-Won;Kim, Won
    • Journal of Korea Water Resources Association
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    • v.37 no.1
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    • pp.31-41
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    • 2004
  • A soil moisture measuring method of hillslope for Korean watershed is developed to configure spatial-temporal distribution of soil moisture. Intensive surveying of topography had been performed to make a digital elevation model(DEM). Flow distribution algorithms were applied and a measurement system was established to maximize representative features of spatial variation. Soil moisture contribution mechanisms of rainfall-runoff process have been derived. Measurements were performed at the right side hillslope of Buprunsa located at the Sulmachun watershed. A Multiplex system has been operated and spatial-temporal soil moisture data have been acquired. Relatively high correlation relationship between flow distribution algorithm and measurement data can be found on the condition of high humidity.