soil survey technology overview n.
Skip this Video
Loading SlideShow in 5 Seconds..
Download Presentation

Loading in 2 Seconds...

play fullscreen
1 / 53


  • Uploaded on

SOIL SURVEY TECHNOLOGY OVERVIEW. Michael A. Wilson Research Soil Scientist USDA-NRCS National Soil Survey Center Lincoln, NE. OBJECTIVES Useful tools for answering questions about soil properties. Soil Survey Office Labs Active C VNIR Portable X-ray Fluorescence Climate stations

I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
Download Presentation


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
    Presentation Transcript
    1. SOIL SURVEY TECHNOLOGY OVERVIEW Michael A. Wilson Research Soil Scientist USDA-NRCS National Soil Survey Center Lincoln, NE

    2. OBJECTIVESUseful tools for answering questions about soil properties • Soil Survey Office Labs • Active C • VNIR • Portable X-ray Fluorescence • Climate stations • Isotic/Spodic • Geophysical tools

    3. SSO Laboratories—Your lab • Field kits provide opportunity to collect limited data to answer specific questions • Not a replacement for NSSC KSSL • Lower accuracy/higher detection limits • Less efficient • Why use field kits? • Check of certain properties as part of map unit evaluation or mapping • Rapid turn around of data • Prescreening pedons for SSL analysis

    4. Types of Analyses • Particle size distribution - hydrometer • Chemical properties • pH • EC • Hach kit • Base saturation • Extractable cations • Salts • CaCO3 equivalent • Gypsum content • Active C • Isotic / Spodic properties

    5. Field methods available to use are documented in this 2009 Manual

    6. Laboratory Safety • Not a trivial matter • Protect yourself and others • Use common sense • OSHA citation

    7. Soil Survey Office Laboratory Safety Manual is available on-line

    8. MSDSMaterial Safety Data Sheet • Information regarding the proper procedures for handling, storing, and disposing of chemical substances • Required to be read, kept, and stored in lab in organized manner

    9. Chemical Hygiene Plan • Document you write for your lab • Policies, procedures, and responsibilities to protect employees from the health hazards of chemicals used • OSHA’s Occupational Exposure to Hazardous Chemicals in Laboratories Standard details requirements of a CHP to protect persons from hazardous chemicals • CHP has required elements

    10. Soil Survey Technologiesto Discuss • Active C • VNIR • Portable X-ray Fluorescence • Spodic Field Kit • Climate Stations • Geophysical tools

    11. Active Carbon Kit C. Stiles, et al., 2011. Validation Testing of a Portable Kit for Measuring an Active Soil Carbon Fraction.Soil Sci. Soc. Am. J. 75:2330–2340

    12. Active Carbon Analysis • Potassium Permanganate -- weak oxidant of organic C • Active (labile) C is the biologically active fraction • Soil Health/Soil Quality Indicator of active food web, microbial biomass, and nutrient cycling • Has been shown to be related to tillage systems • Early indicator of C degradation

    13. Active C:Total C Ratio Acitive C related to total C but not consistently

    14. Visible Near IfraRed Diffuse Reflectance Spectroscopy • Chemical bonds interact with Visible and IR energy • Different bonds – different wavelengths Atomic Bond Energy Vibration Bending Rotation

    15. Visible Near IfraRed Spectroscopy • Amount of interaction proportional to quantity • Measurement is spectrum • Statistical prediction based on spectral library • Soil minerals • Si-O bonds • Al-O bonds • Bond energy varies with mineralogy • Organic matter • C-O bonds • C-H bonds • VNIR –Measures spectral signatures of materials defined by their reflectance as a function of wavelength. • Signatures are due to electronic transitions of atoms and vibrational stretching and bending of structural groups of atoms that form molecules and crystals.

    16. Visible to Near Infrared Diffuse Reflectance Spectroscopy • VNIR-DRS • Measures reflectance at a wide range of wavelengths • 350-2500 nm • Rapid: 100 readings per second • Interaction with sample composition and matrix produces diffuse reflectance Spectral Radiometer Fiber Optic Light Source Diffuse Reflectance Soil

    17. Data Collection • Portable VNIR spectrometers • 1 per MO • Spectra measurements • ~1 min/depth • Predictive models developed at SSL • Organic and inorganic C • Other properties as appropriate

    18. Benefits of VNIR • Little or no sample prep • Field analysis of moist soils may be possible • Possible to collect spectra in the field • Spectra can be used to predict multiple properties • Useful for rapid collection of data on many samples • Traditional lab methods more accurate for a limited number of samples

    19. Clay Content Measured Clay (%) Measured Clay (%) Calibration Test Data Estimated Clay (%) Estimated Clay (%)

    20. Cation Exchange (NH4OAc) Measured CEC (meq 100g-1) Measured CEC (meq 100g-1) Calibration Test Data Estimated CEC (meq 100g-1) Estimated CEC (meq 100g-1)

    21. Soil Organic Carbon (Leco) R2 = 0.9 PLSR R2 = 0.82 RMSE = 0.15 RPD = 2.4

    22. Portable X-ray Fluorescence Spectroscopy Different Manufacturers Bruker Tracer IV-SD Oxford X-MET 5000 Olympus Innov-X Delta RXF Thermo Scientific Niton XL2 GOLDD QSX Quickshot

    23. XRF VNIR X-ray fluorescence (XRF) is used to detect and measure the concentration of elements in substances. Fluorescence - phenomena of absorbing incoming radiation and re-radiating it as lower-energy radiation.

    24. Key Point: Atoms fluoresce at specific energies when excited by X-rays. Energy source: X-ray tube or radioisotope X-ray fluorescence (XRF) Subsequently, electrons of higher energy orbitals fall into the lower orbitals. A fluorescent photon with a characteristic energy is released. When exposed to x-rays, electrons are ejected from inner orbitals

    25. Facts of Portable XRF • Excitation source is either: • X-ray tube with target of Ag (silver), Ta (tantalum), Au (gold), Rh (rhodium), W (Tungston) • Radioisotope (e.g., Fe-55, Co-57, Cd-109) • Analysis covers area of 1 cm2 to a depth of approximately 2mm • Minimum set up and calibration required (Factory Calibrated with alloy chip) • Proper training is essential--User must understand the dangers of x-rays and fundamentals of radiation protection

    26. Advantages of Portable XRF • Rapid field analysis and ease of use. • Portable and easily transported to job sites; can check on an airplane as baggage or carry-on • Delivers qualitative and/or quantitative multi-element analysis; simultaneous determination • Can be used on many different samples - solids, powders, liquids, etc. • Little or no sample preparation required

    27. Very difficult to detect or quantify lighter elements e.g., Si, Al, Li, Be, P, B, C Elements quantified by XRF

    28. Limitation of Portable XRF PXRF is viewed by EPA as a screening method

    29. Multiple applications in soils survey for element specific measurements • Geographic profiling of elemental constituents in profiles • Target elemental concentration in calcic, gypsic, spodic, placic horizons • Mapping/spatial variability of contaminants across landscape • Assist in selection of sites for sample collection

    30. Spodic Field Kit • HumicFulvic Color—indicates translocation and accumulation of organic complexes in spodic horizons. (Holmgren and Holzhey, 1984). • KOH extraction of Al – Comparable to acid oxalate extractable Al If KOH-Al >2%, P retention is generally 100% and likely andic soil properties. In Spodosols, a level of 0.7% KOH-Al has been found to indicate the presence of a spodic horizon if the ratio of Al in the spodic material to that in the E horizon is >2.

    31. Climate Stations and Data Loggers • Deb Harms • Data loggers – • Compact, battery-powered device to records measurements at set intervals over a period of time. • Record temperature, relative humidity, differential pressure, light intensity, water level, soil moisture, rainfall, wind speed and direction.

    32. Climate StationApplications to Soil Survey • To define the line between soil climate regimes • Supporting data to determine landscape and soil hydrology   • Determine soil temperature vs air temperature off-sets for the region

    33. Soil Climate Stations • Measure soil temperature and soil moisture by volume • Can include air temperature sensors and tipping-bucket rain gauge • The stations are self contained and battery powered charged with a solar panel • Store the data up to one year and then need to be manually downloaded.    Possible to purchase cell phone system so the sites can be downloaded remotely.

    34. Wells/Piezometers

    35. Geophysical Methods • Jim Doolittle (PA) • Wes Tuttle (NC) • Several states have equipment and operators Ground-Penetrating Radar (GPR) Electromagnetic Induction (EMI)

    36. Ground Penetrating RadarPrincipal Soil Survey Uses • Determine the presence, depth, and lateral extent of subsurface horizons, stratigraphic and lithologic layers. • Improve interpretations by providing estimates of soil map unit composition. • Characterize spatial and temporal variations in soil properties.

    37. Use of GPR for soil survey investigations is limited by the medium. • In the conterminous USA, only 22 % of the soils are considered well suited to GPR. About 36 % of the soils are considered poorly suited to GPR,

    38. GPR ApplicationCharacterization of Peatlands

    39. Rock fragments limit the effectiveness of conventional soil survey tools. GPR Application-- Soil Depth Determinations • One of the most effective uses of GPR has been to chart bedrock depths and determine the taxonomic composition of soil map units based on soil-depth criteria.

    40. GPR Application Characterizing Subaqueous Soils

    41. Subaqueous SoilsGPR can provide data on fresh water depths, subbottom topographies, and sediment types.

    42. GPR Application Preferential Flow Paths The movement of water through soil is not uniform and is strongly influenced by soil layering. Discontinuities provide narrow flow paths that account for a significant proportion of the water and contaminants moved thru the soil.

    43. GPR Application Depth and Continuity of Water Restricting Layers Cisne - Fine, smectitic, mesic Mollic Albaqualfs Darley - Fine, kaolinitic, thermic Typic Hapludults

    44. Electromagnetic Induction (EMI)

    45. The electrical conductivity of soils is influenced by: • the type and concentration of ions in solution. • the amount and type of clays in the soil matrix. • the volumetric water content. • the temperature and phase of the soil water. THE APPARENT CONDUCTIVITY OF SOILS WILL INCREASE WITH INCREASING: • Water • Clay • Soluble salt

    46. EMI ApplicationHigh-Intensity Soil Surveys Identification and delineation of small inclusions of dissimilar soils within generalized soil polygons.

    47. EMI Application Characterization of spatial soil variability EMI can provide a level of resolution not practical with traditional soil survey tools and methods

    48. EMI Application Identifying soil-hydrologic-landscape units Menfro – Fine-silty, mixed, superactive, mesic Typic Hapludalfs

    49. EMI Application Spatiotemporal variations in ECa associated with changes in soil moisture.

    50. EMI Application Characterizing and mapping anthropogenic soils