Lecture 4 soil moisture Flashcards
What can remote sensing be used for - soil moisture related
▪ Map soil aerial coverage
▪ Important for geomorphology, hydrology (runoff, infiltration) farmers can understand soil deficiencies and soil moisture – drought indicators.
▪ Estimate soil physiochemical properties ▪ e.g., soil organic carbon (SOC), salinity, composition (clay, sand), nitrogen, soil moisture
Factors influencing reflectance (soil moisture)
- Soil moisture content
- Organic content
- Structure (surface roughness and texture)
- Mineralogical composition (e.g. Iron oxide content) Important to remember that the coverage of bare earth varies over time (e.g. land management practices, phenological cycle).
Soil reflectance info
Soil reflectance Increases with wavelength.
Soil reflectance can be : ▪ Surface reflectance ▪ Volume scattering
What is soil moisture important for?
▪ plant growth and soil health ▪ Hydrological system (water store) ▪ local weather (evaporation & plant evapotranspiration) indicator of drought.
What does moisture do to the surface
reduced brightness/reflectance of the surface
Water ‘coats’ soil particles and fills in airspaces – reflectance decreases absorption increases.
▪ reduces the amount of multiple scattered light
▪ this influences the visible and NIR wavelengths and reduces reflectance\ brightness
▪ Increases absorption
▪ impacts the shortwave infrared (SWIR) where water absorption is strongest
Why use microwaves for soil moisture
Microwave sensors are typically used to measure soil moisture content ▪ Microwave wavelengths are sensitive to soil moisture ▪ Operate day and night and can see through cloud cover.
Different soils have different particle sizes - why is this important
Particle size influences (e.g.)
▪ Susceptibility to wind & water transport
▪ Leaching potential – how tightly packed soil is
▪ Water holding capacity
▪ Exchangeable nutrient supply
Observed trend - smaller the particle size the larger the reflectance
▪ Stronger at longer (e.g. SWIR) wavelengths than for shorter (visible)
▪ Smaller soil particles result in increased volume scattering
Smaller particles closer together – more volume scattering
Work out mineral compositions from soils - example Iron oxide
gives soil its red colour - reflects in the red part of the spectrum and absorbs blue and green and NIR wavelengths.
Why would we choose to measure relationship between EMR and Water?
- water quality, sediment content - rivers, O2, temperature, climate and salinity. Areas nearest coasts. river outflows have lower salinity.
Is water reflected transmitted or absorbed?
Visible part of the spectrum - reflected, other parts it is absorbed unless water is rough (but very little). Increased sediment increases reflectance.
the majority of EMR incident on water are either absorbed or transmitted ▪ Clear water has very low reflectance (< 3%) over the visible, NIR, and SWIR regions.
▪ Higher reflectance in the blue and green wavebands.
▪ Almost no reflectance in wavelengths > (greater than 0.8 µm.
How would water appear in a NIR image
water appears black/dark, low reflectance, high absorption and land surface appears lighter.
Vegetation within water – reflectance above surface but lower.
A sharp contrast between water and land boundary * Useful for masking out water bodies or mapping floods.
What types of reflectance occur on water
- Surface reflectance – sun glint
- Volume reflectance – dependent on sediment within
- Bottom reflectance – depends on depth
What causes sun glint
surface reflectance caused by specular reflectance
What does volume reflectance help with?
- Volume reflectance provides information on water quality (related to material in the water)
- Only volume reflectance contains information relating to water quality. For deep (> 2 m) clear water bodies, volume reflectance is very low (6-8 %) and is confined to the visible wavelengths.
What are the factors affecting reflectance of water?
▪ Depth of water and substrate below the water (if the substrate is coral reef - reflects more, rocky would reflect less)
▪ Material within water: - sediment - water chlorophyll content (absorbs energy in blue and red - reflects in green)
▪ Surface roughness of water