Measurement of Water Level, Electrical Conductivity, and Sediment Surface Level Using Time Domain Reflectometry

Σχετικά έγγραφα
2000cm 3 (1) Derby m s m w m a V s. : w = m w /m s : θ= V w / V t (1)

GS3. A liner offset equation of the volumetric water content that capacitance type GS3 soil moisture sensor measured

; +302 ; +313; +320,.


Hydrologic Process in Wetland

Reaction of a Platinum Electrode for the Measurement of Redox Potential of Paddy Soil

Comparison of Evapotranspiration between Indigenous Vegetation and Invading Vegetation in a Bog

Development of Automated Suction Controlled Flux Sampler for Unsaturated Sandy Soil

1, +,*+* + +-,, -*, * : Key words: global warming, snowfall, snowmelt, snow water equivalent. Ohmura,,**0,**

LUNGOO R. Control Engineering for Development of a Mechanical Ventilator for ICU Use Spontaneous Breathing Lung Simulator LUNGOO

1 (forward modeling) 2 (data-driven modeling) e- Quest EnergyPlus DeST 1.1. {X t } ARMA. S.Sp. Pappas [4]

The martingale pricing method for pricing fluctuation concerning stock models of callable bonds with random parameters

DATA SHEET Surface mount NTC thermistors. BCcomponents

Neutralization E#ects of Acidity of Rain by Cover Plants on Slope Land

Reviewing classical studies in soil physics. Analysis of the vertical downward flow of water through a two layered soil By S. Takagi.

* ** *** *** Jun S HIMADA*, Kyoko O HSUMI**, Kazuhiko O HBA*** and Atsushi M ARUYAMA***

Physical and Chemical Properties of the Nest-site Beach of the Horseshoe Crab Rehabilitated by Sand Placement

GAUGE BLOCKS. Grade 0 Tolerance for the variation in length. Limit deviation of length. ± 0.25μm. 0.14μm ±0.80μm. ± 1.90μm. ± 0.40μm. ± 1.

GF GF 3 1,2) KP PP KP Photo 1 GF PP GF PP 3) KP ULultra-light 2.KP 2.1KP KP Fig. 1 PET GF PP 4) 2.2KP KP GF 2 3 KP Olefin film Stampable sheet

Soil Temperature Change and Heat of Wetting during Infiltration into Dry soils

By R.L. Snyder (Revised March 24, 2005)

Calculating the propagation delay of coaxial cable


Application of Soil Physics to Rainwater Dynamics at Forested Hillslopes

ΕΙΣΑΓΩΓΗ ΣΤΗ ΣΤΑΤΙΣΤΙΚΗ ΑΝΑΛΥΣΗ

CorV CVAC. CorV TU317. 1

Si + Al Mg Fe + Mn +Ni Ca rim Ca p.f.u

Bulletin 1489 UL489 Circuit Breakers

Homework 8 Model Solution Section

*,* + -+ on Bedrock Bath. Hideyuki O, Shoichi O, Takao O, Kumiko Y, Yoshinao K and Tsuneaki G

MMCX SERIES Microminiature Coaxial Connectors

Trace gas emissions from soil ecosystems and their implications in the atmospheric environment

Optimizing Microwave-assisted Extraction Process for Paprika Red Pigments Using Response Surface Methodology

Changes and Issues of Consolidation Techniques of Peaty Arable Land in Hokkaido

Data Sheet High Reliability Glass Epoxy Multi-layer Materials (High Tg & Low CTE type) Laminate R-1755V Prepreg R-1650V

Quantitative chemical analyses of rocks with X-ray fluorescence analyzer: major and trace elements in ultrabasic rocks

Metal-free Oxidative Coupling of Amines with Sodium Sulfinates: A Mild Access to Sulfonamides

Έλεγχος και Διασφάλιση Ποιότητας

BMA SERIES Subminiature Blind Mate Connectors

ΘΕΩΡΗΤΙΚΗ ΚΑΙ ΠΕΙΡΑΜΑΤΙΚΗ ΙΕΡΕΥΝΗΣΗ ΤΗΣ ΙΕΡΓΑΣΙΑΣ ΣΚΛΗΡΥΝΣΗΣ ΙΑ ΛΕΙΑΝΣΕΩΣ

Retrieval of Seismic Data Recorded on Open-reel-type Magnetic Tapes (MT) by Using Existing Devices

High Speed, Low Loss Multi-layer Materials

Ελαφρές κυψελωτές πλάκες - ένα νέο προϊόν για την επιπλοποιία και ξυλουργική. ΒΑΣΙΛΕΙΟΥ ΒΑΣΙΛΕΙΟΣ και ΜΠΑΡΜΠΟΥΤΗΣ ΙΩΑΝΝΗΣ

Experimental Study of Water Redistribution Measurement in the Model Earthen Wall and its Numerical Analysis

ect of Modified Wheat Starches on the Textural Properties of Baked Products, such as Cookies

Math 6 SL Probability Distributions Practice Test Mark Scheme

ENSINGER High-temperature plastics. Material standard values.

E#ects of Drying on Bacterial Activity and Iron Formation in Acid Sulfate Soils

Electronic Supplementary Information

Q L -BFGS. Method of Q through full waveform inversion based on L -BFGS algorithm. SUN Hui-qiu HAN Li-guo XU Yang-yang GAO Han ZHOU Yan ZHANG Pan

Handbook of Electrochemical Impedance Spectroscopy

Conductivity Logging for Thermal Spring Well

Οι απόψεις και τα συμπεράσματα που περιέχονται σε αυτό το έγγραφο, εκφράζουν τον συγγραφέα και δεν πρέπει να ερμηνευτεί ότι αντιπροσωπεύουν τις

Design Method of Ball Mill by Discrete Element Method

IPSJ SIG Technical Report Vol.2014-CE-127 No /12/6 CS Activity 1,a) CS Computer Science Activity Activity Actvity Activity Dining Eight-He

Creative TEchnology Provider

J.R. Philip and D.A. de Vries

Soil Environment Monitoring by Multi-frequency Electromagnetic Sounding

Study on Re-adhesion control by monitoring excessive angular momentum in electric railway traction

1. Ηλεκτρικό μαύρο κουτί: Αισθητήρας μετατόπισης με βάση τη χωρητικότητα

SMB SERIES Subminiature Coaxial Connectors

Answers - Worksheet A ALGEBRA PMT. 1 a = 7 b = 11 c = 1 3. e = 0.1 f = 0.3 g = 2 h = 10 i = 3 j = d = k = 3 1. = 1 or 0.5 l =

SPBW06 & DPBW06 series

SMC SERIES Subminiature Coaxial Connectors

Daewoo Technopark A-403, Dodang-dong, Wonmi-gu, Bucheon-city, Gyeonggido, Korea LM-80 Test Report

ΙΕΥΘΥΝΤΗΣ: Καθηγητής Γ. ΧΡΥΣΟΛΟΥΡΗΣ Ι ΑΚΤΟΡΙΚΗ ΙΑΤΡΙΒΗ

Figure 3 Three observations (Vp, Vs and density isosurfaces) intersecting in the PLF space. Solutions exist at the two indicated points.

Toward the Quantitative Study of Hydrothermal Systems An Approach to Understand Hydrothermal Systems

SMC SERIES Subminiature Coaxial Connectors

Surface Mount Multilayer Chip Capacitors for Commodity Solutions

RECIPROCATING COMPRESSOR CALCULATION SHEET

Characterization Report

Table 2 Suggested prediction methods to use for a given set of available input parameters per each examined soil hydraulic property) a.

Discontinuous Hermite Collocation and Diagonally Implicit RK3 for a Brain Tumour Invasion Model

4 Way Reversing Valve

ΜΑΘΗΜΑΤΙΚΗ ΠΡΟΣΟΜΟΙΩΣΗ ΤΗΣ ΔΥΝΑΜΙΚΗΣ ΤΟΥ ΕΔΑΦΙΚΟΥ ΝΕΡΟΥ ΣΤΗΝ ΠΕΡΙΠΤΩΣΗ ΑΡΔΕΥΣΗΣ ΜΕ ΥΠΟΓΕΙΟΥΣ ΣΤΑΛΑΚΤΗΦΟΡΟΥΣ ΣΩΛΗΝΕΣ ΣΕ ΔΙΑΣΤΡΩΜΕΝΑ ΕΔΑΦΗ

Assalamu `alaikum wr. wb.

Multilayer Chip Inductor

20/01/ of 8 TOW SSD v3. C 2.78AC Σ Cumul. A*C. Tc 1 =A14+1 =B14+1 =C14+1 =D14+1 =E14+1 =F14+1 =G14+1 =H14+1 =I14+1 =J14+1 =K14+1

Review Test 3. MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

Anisotropy of Drainable Macropores in Andosols and Alluvial Soils

RSDW08 & RDDW08 series

Transient Voltage Suppressor

ΡΥΠΑΝΣΗ ΕΠΙΦΑΝΕΙΑΚΩΝ Υ ΑΤΩΝ ΑΠΟ ΙΑΘΕΣΗ ΒΑΡΕΩΝ ΛΥΜΑΤΩΝ (ΛΥΜΑΤΩΝ ΑΡΝΗΤΙΚΗΣ ΑΝΩΣΗΣ)

SUPPLEMENTAL INFORMATION. Fully Automated Total Metals and Chromium Speciation Single Platform Introduction System for ICP-MS

SEN TRONIC AG A AB 93 :, C,! D 0 7 % : 3 A 5 93 :

Influence of Flow Rate on Nitrate Removal in Flow Process

Experimental Study of Dielectric Properties on Human Lung Tissue

SMD Transient Voltage Suppressors

Isotopic and Geochemical Study of Travertine and Hot Springs Occurring Along the Yumoto Fault at North Coast of the Oga Peninsula, Akita Prefecture

Error ana lysis of P2wave non2hyperbolic m oveout veloc ity in layered media

Tanzania. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Problem 3.1 Vector A starts at point (1, 1, 3) and ends at point (2, 1,0). Find a unit vector in the direction of A. Solution: A = 1+9 = 3.

Buried Markov Model Pairwise

4 Way Reversing Valve

ΑΡΙΣΤΟΤΕΛΕΙΟ ΠΑΝΕΠΙΣΤΗΜΙΟ ΘΕΣΣΑΛΟΝΙΚΗΣ

High Performance Voltage Controlled Amplifiers Typical and Guaranteed Specifications 50 Ω System

SCOPE OF ACCREDITATION TO ISO 17025:2005

TURCK Pressure Instrumentation

Study on the Strengthen Method of Masonry Structure by Steel Truss for Collapse Prevention

Transcript:

J. Jpn. Soc. Soil Phy. No. +*2 p. -1./ **2 * * * Meaurement of Water evel Electrical Conductivity and Sediment Surface evel Uing Time Domain Reflectometry Hideki M IYAMOTO* Jiro C HIKUSHI* and Taek-Keun O H* * Biotron Intitute Kyuhu Univerity 0 +* + Hakozaki Higahi-ku Fukuoka 2+ 2/2+ Japan Abtract Time domain reflectometry (TDR) ha been draing a lot more attention a a ay to identify the interface in beteen di# erent dielectric media. To monitor ater level ( h ) ith electrical conductivity ( ) and iment urface level ( h ) in river by applying TDR e developed a mathematical model to evaluate thee propertie and verified it e# ectivene by meauring the dielectric contant of conductive fluid media and a oil material (and) uing TDR probe ith di# erent length. Although the determination of h in extremely high-conductive media a technically incompleted e could uccefully determine h and h ith a probe in moderateconductive media. Judging from the relatively good agreement beteen propertie evaluated from the model and oberved data e concluded the TDR meaurement could be ueful to evaluate h and h ith u$ cient accuracy for practical ue ithin an appropriate conductive range. In actual application of TDR to a river monitoring the calibration of the probe u mut be required to conduct accurate meaurement ba of the model. Key ord : Time domain reflectometry Microave Dielectric contant Water level Electrical conductivity Sediment urface level + Time Domain Re- flectometry TDR TDR TDR * 2+ 2/2+ 0 +* + :

38 +*2 **2 +331 Krohne EndreHauer Vega TDR +2. **- TDR TDR + TDR TDR Fig. + Schematic diagram of a TDR aveform Cataldo in inerting a probe partly into a dielectric et al. **0 ; Thomen et al. *** ; **- material. B eb t* t A-B t+ Thomen et al. *** ; Yu and Yu **0 ; +330 r A TDR B e t TDR /+ t t* ct e TDR 2 + c -*. +* m TDR rf A B TDR e Heimovaara et al. +33/ t RRc R TDR TDR t Rc + A B **- m TDR hb m + TDR + A e e A

: 39 n n n n A B h h e e h A A B B A a m h TDR Moret et al. **. a b h Yu and Yu **0 h m TDR Yu and Yu **0 + A B A B Sm h h b a * e e e q h h h + q q + b h b+ e h q h e baln b B b b n A Bn A b B b b b b a a TDR+** Campbell Scientific TDR a b +** *./ V +. m -** p h/ aln balnlnln * exp - b b - -+ +1/. Topp et al. +32 ; Rob- inon et al. **-b GHz Robinon et al. **-a

40 +*2 **2 * mm +*. m *+. m *.2. m *31. m *.2. m -- *.2. m *31. m */. m +*. m Fig. Schematic diagram of experimental tu #. *31. m +/ *..2 m - -/ *..2 m. mm +* mm *. +*/ *./3 mm **1. m */. m +/ DW TW TDR CaCl *.**2 *.*+0 *.*.* *.*2.. Sm. m + * ++ * ** * */ +2 *..2 m *./+ m + - - - *.*++ Sm +32+ m *. 31 m *./- m m. TDR.+ TDR+** TDR+**.++ TDR PCTDR *.2. m TDR h */. m- PCTDR DW t t t + *.** Sm t t. m mm. S m + * 31 / * ** -

: 41 - *.2. m */. m TDR Fig. - TDR aveform meaured ith a *.2. -m long probe in di# erent conductive olution. / Fig. / *.2. m *31. m h Water level ( h ) for the quare root of dielectric contant ( ) meaured ith a *.2. -m long probe and a *31. -m long probe in di# erent olution. Broken line in the figure indicate theoretical value etimated from eq. (/).. *.2. m h TDR Fig.. TDR aveform meaured ith a *.2. -m long probe in di# erent level ( h) of ditilled ater. t t.+ / *..2 m *. 31 m TDR t e h t + *.** Sm +/ 2. 3*1. *.2. m 3*1... h t t h *+. m + *32. m t t t + + h t t * + t t + +

42 +*2 **2 0 *.2. m 1 b h Fig. 1 A parameter b for electrical conductivity Fig. 0 Electrical conductivity ( e# ) meaured of fluid media ( ). ith a *.2. -m long probe for ater level ( h) in di# erent fluid media. Fitting function of eq. ( 2) for experimental data 0 1 plot are expre by broken line. b b a b e *. + *. 3-* + h. / 2 a b h + */. mm.+- *.2. m h 0 0 h.+. *.2. m -. h t b TDR b

: 43 2 h Fig. 2 Etimated electrical conductivitie of fluid media ( ) for relative ater level ( h/ ). Broken line in the figure indicate actual electrical conductivity of each fluid medium. +2 * *++ +32+ +. Sm Dalton and van Genuchten +320 TDR m b ***/. **++. ***. + + **++. Sm +*. 3 h Fig. 3 Maximum probe length ( ) being applicable to relative ater level ( h/ ) meaurement. *.**0++ 3 *.2. m a a b *.*/* *. +** *.** Sm..2-. m.2-. m *.2. m TDR +* *.2. h m t t +

44 +*2 **2 +* *.2. m ++ *.2. m *31. m h TDR Fig. +* TDR aveform meaured ith a *.2. - h m long probe in di# erent thickne of oil iment. Fig. ++ Sediment thickne ( h ) for the quare root of dielectric contant ( ) meaured ith a *.2. -m long probe and a + *+*. mm t *31. -m long probe. Solid line in the figure in the figure indicate theoretical *32. m value etimated from eq. ( +. ). t h ++ *..2 m h TDR *31. m *.2. m - - */+. m m -/ 1*/. *31. m - - */-. m m +/ 12. /. TDR e h ++ CaCl - ++ TDR TDR Cataldo A. Tarricone. Attiviimo F. and Trotta

: 45 A. (**0) : Simultaneou meaurement of dielec- Friedman S.P. (**-a) : A revie of advance in tric propertie and level of liquid uing a TDR dielectric and electrical conductivity meauremethod. J. Hydrology in pre and available at ment in oil uing time domain reflectometry. doi : +*. +*+0 /j.meaurement.**0. ++.**0. Vadoe Zone J. :....1/. +330 : TDR Robinon D.A. Schaap M. Jone S.B. Friedman S.P. +2 +0- +0.. and Gardner C.M.K. (**-b) : Conideration for Dalton F.N. and van Genuchten M.Th. ( +320) : The improving the accuracy of permittivity meauretime-domain reflectometry method for meaurcalibration ment uing time domain reflectometry : Air-ater ing oil ater content and alinity. Geoderma -2 : e# ect of cable length. Soil Sci. Soc. -1 /*. Am. J. 01 : 0 1*. Heimovaara T. J. Focke A.G. Bouten W. and Vertraten J.M. ( +33. ) : Aeing temporal variation in oil ater compoition ith time domain reflectometry. **- : in **- : ++ +/ Soil Sci. Soc. Am. J. /3 : 023032. Thomen A. Hanen B. and Schelde K. (***) : Ap- +32+ : plication of TDR to ater level meaurement. J. - pp. +00 +03 Hydrology -0 (-. ) : / /2. **- : Topp G.C. Davi J.. and Annan A.P. ( +32 ) : Elec- MS TODAY + 2 : -. tromagnetic determination of oil ater content Moret D. ópez M.V. and Arrúe J.. (**.) : TDR uing TDR : I. Application to etting front and application for automated ater level meaure- teep gradient. Soil Sci. Soc. Am. J..0 : 01 012. ment from Mariotte reervoir in tenion dic Yu X. and Yu X. (**0) : Meaurement of imulated infiltrometer. J. Hydrology 31 : 3 -/. cour by time domain reflectometry Proc. TDR **- : TDR 3- : /10/. **0. available on line at http : //engineering. purdue.edu/tdr/paper. Robinon D.A. Jone S.B. Wraith J.M. Or D. and TDR CaCl TDR : **1 + : **2 +.