Laboratory Testing and Calibration of Vertically Oriented TDR Soil Moisture Sensors By: Phillip McFarland.

Slides:



Advertisements
Similar presentations
Models for heat and moisture transport in a microwave oven Andrew Hill & Prof. C.J. Budd University of Bath, UK Greg Hooper CCFRA, UK Faraday CASE award.
Advertisements

TURKEY AWOS TRAINING 1.0 / ALANYA 2005 SOIL MOISTURE MEASUREMENT.
Measurement methods for soil moisture and plant water relations
Outline More Wikipedia stuff Where were we? Measuring soil wetness
Water Content Measurement Methods and Field Applications
School of Natural Resources University of Nebraska  Lincoln Soil Moisture Monitoring, Data, and Products in Nebraska Eric Hunt, Brian Fuchs, Mark Svoboda.
Jump to first page Lecture 4 n Below ground processes n Water reaches the ground beneath a forest as throughfall (direct raindrop passage through the canopy,
Matt Galloway. 2 Volumetric water content sensors measure volumetric water content, right?
Why does my soil moisture sensor read negative? Improving accuracy of dielectric soil moisture sensors Douglas R. Cobos, Ph.D. Decagon Devices and Washington.
STABILITY ANALYSIS IN PRESENCE OF WATER Pore pressures Rainfall Steady state flow and transient flow.
NOAA-CREST GPR Study Eric Harmsen, Associate Researcher Agricultural and Biosystems Engineering.
Ground Penetrating Radar (GPR) GPR technology can be used to determine depth to bedrock and or water table, locate buried ordinance at gunnery ranges,
Soil Physics 2010 Outline Website notice Where were we? Measuring soil wetness with TDR Water.
Soil Moisture Measurement for Irrigation Scheduling Sanjay Shukla Agricultural and Biological Engineering UF-IFAS.
Soil Water Measurement
Characterization of the Soil Liquid Phase
Washington State University
Literature Survey on Sensors ECE5320 Mechatronics Literature Survey on Sensors Topic: Time Domain Reflectometry Sensor Prepared by: Ricardo Estevez Dept.
Soil Moisture Estimation Using Hyperspectral SWIR Imagery Poster Number IN43B-1184 D. Lewis, Institute for Technology Development, Building 1103, Suite.
TDR (Time Domain Reflectometers). Pictures of different TDR probes
Non-destructive evaluation of civil structures using electromagnetic waves Pablo Juan-García, Thesis Advisor: Josep M. Torrents Department of Electronic.
Lawrence H. Haselmaier, Jr. Computer Scientist Naval Oceanographic Office 7 August 2014.
University of Nebraska Carbon Sequestration Program.
Humidity - Humidity sensors - Vapour pressure and dew point temperature - Soil moisture sensors - Leaf wetness sensors.
Soil Water Potential Peter Cull ICT International.
Averaging water content and electrical conductivity of a layered soil using time domain reflectmetry Hiroyuki Ochiai, and Kosuke Noborio School of Agriculture,
Evaluation of Ground-Penetrating Radar-Derived Soil Moisture Contents for Use with Unsaturated Numerical Flow Models Eric Harmsen Hamed Parsiani.
Installation and Calibration of Moisture Probes Ben Worel Len Palek Minnesota Department of Transportation.
CEMTREX, INC. MODCON SYSTEMS LTD NIR Systems July 2010.
Remote Sensing and geophysical Methods for Evaluation of Subsurface Conditions Matt Houston.
Soil Water Reading: Applied Hydrology Sections 4.1 and 4.2 Topics
SACE Stage 2 Physics Motion in 2 Dimensions.
Validation of AMSR-E Soil Moisture Estimation in Mongolia and A Renewal Plan of Ground-based Monitoring Instruments Ichirow Kaihotsu (Hiroshima University)
EM propagation paths 1/17/12. Introduction Motivation: For all remote sensing instruments, an understanding of propagation is necessary to properly interpret.
Geology 5660/6660 Applied Geophysics 26 Feb 2014 © A.R. Lowry 2014 For Fri 28 Feb: Burger (§8.4–8.5) Last Time: Industry Seismic Interpretation.
Moisture impact on building rocks - the laboratory and in situ investigations FIDRÍKOVÁ D., KUBIČÁR Ľ. Institute of Physics SAS, Bratislava, Slovakia The.
Sensor Technology Soil Moisture Sensor -By Amrit Gautam (TI13S1) A soil water sensor is an instrument which, when placed in a soil for period of time,
TDS8000 and TDR Considerations to Help Solve Signal Integrity Issues.
Real-Time Bridge Scour Monitoring: Recent Technological Development Present at Ohio Transportation Engineering Conference Oct 23-24, 2007 Bill X. Yu and.
UNDERSTANDING VARIATION WILL REDUCE YOUR WATER COSTS ANDY BROWN TORO EUROPE.
Lecture Notes Applied Hydrogeology
COSMOS use at the Southern Sierra Critical Zone Observatory 3 rd Annual COSMOS Workshop Matthew Meadows Sierra Nevada Research Institute University of.
CE 394K.2 Hydrology Infiltration Reading AH Sec 5.1 to 5.5 Some slides were prepared by Venkatesh Merwade Slides 2-6 come from
William Crosson, Ashutosh Limaye, Charles Laymon National Space Science and Technology Center Huntsville, Alabama, USA Soil Moisture Retrievals Using C-
Introduction and Background In civil engineering and geotechnical engineering, dry density of soil and water content of soil are two parameters used for.
DRAINMOD APPLICATION ABE 527 Computer Models in Environmental and Natural Resources.
Soil moisture sensor sm-300. Contents Introduction Features SM300 working procedure Installation Calibration Specification.
Soil Water Relationships
Advanced Inspection Techniques for Monitoring Cable Aging Module 3 Dr. John H. Bickel Evergreen Safety & Reliability Technologies, LLC.
Motivation: In civil engineering and geotechnical engineering, dry density of soil and water content of soil are two parameters used for construction control.
1 Rosalia Daví 1 Václav Vavryčuk 2 Elli-Maria Charalampidou 2 Grzegorz Kwiatek 1 Institute of Geophysics, Academy of Sciences, Praha 2 GFZ German Research.
 Installation. Schematic of a weighable gravitation lysimeter.
BASIC SOIL PLANT WATER RELATIONS
© 2014 Pearson Education, Inc. Chapter 5 Water and Seawater Salinity.
Consider following problem Want to measure temperature range of: -15 o C < T 1 < 35 o C. Reference junction, T 2, = 0 o C. Output must be in range of -5Volts.
Ajaya Kumar Kavala Research Scholar Department of Physics IIT Patna Technique for measuring the Dielectric constant using open ended coaxial cable in the.
G. S. Campbell, C. S. Campbell, D. R. Cobos and M. G. Buehler
Geology 5660/6660 Applied Geophysics 04 Apr 2016
Soil-Water-Plant Relationships A. Background 1. Holdridge Life Zones 1.
Antennas/Antenna Arrays
Active Microwave Remote Sensing
By ASST. Prof. DR. ASEEL BASIM
Outline Website notice Where were we? Measuring soil wetness with TDR
Methods Used to Determine Hydraulic Conductivity
ECV Requirements Wolfgang Wagner.
IEEE Regulatory AHC Power Measurement Method
The propagation of waves in an inhomogeneous medium
MSU Agriculture Innovation Day
Compaction Process in the Field
A projectile launched at an angle
Presentation transcript:

Laboratory Testing and Calibration of Vertically Oriented TDR Soil Moisture Sensors By: Phillip McFarland

Project Recap: Soil Moisture – agricultural, hydro-geological modeling and corrections to groundwater gravity measurements. TDR – time domain reflectometry VWC – volumetric water content

Principles of TDR Explanation of “Relative Permittivity”: Maxwell: Applications of Relative Permittivity: Ledieu Equation for VWC:

TDR Waveforms

Waveform Interpretation

Horizontally Oriented Soil Moisture Sensor Probes Proven technology Very accurate VWC measurement Little or no calibration required Destructive to soil In situ TDR device required Costly Limited sample volume per probe

Development of a Vertically Oriented TDR Probe System Challenges: Calibration of probe connectors Larger sample volume Average VWC over several layers v. local measurement at each layer Unknown soil constituents may deflect probe installation (i.e. buried stones) Best material for waveguides Possible Advantages: Easy installation Cost effective Fewer TDR devices required to survey a large land area. Especially when less frequent measurements are needed.

First Attempt!! Results: 38% error!! Probe calibration needed Interesting variations in pulse reflection from connectors Probe calibration needed Probe connector offset constant needed

Theory of Connector Calibration

Calibration Method 20 probe pairs used 4 pairs @ lengths: 28, 24, 20, 16 and 8 in. TDR measurements made in air and DI water 2 measurements made with each pair of waveguides in each medium with each connector 160 TDR measurements total made Relative permittivity of water and air known Measurements compared with theoretical values Probe constant isolated empirically

Results of Calibration Electrical path length constant of waveguide connectors was used to correct previous data collected Average % error decreased by nearly 32%

What’s Next Develop a field ready model Further test existing and new probes and connectors in a wider variety of conditions Implement a comprehensive soil moisture system around gravity measurement sites Use reliable soil moisture information to correct gravity ground water measurements