|
|
|
Land Management & Natural
Hazards Unit |
SOIL |
|
|
|
Soil
Atlas of |
|||||
|
|
|
Digital mapping -the future By using geographic information systems (see Page 97), global positioning systems (GPS) and information collected by remote sensing (i.e. sensors and cameras mounted on aircraft and satellites) to help create maps in the field, vast improvements in consistency, speed of production and accuracy will be realized. When soil is not covered by vegetation, aerial photographs and satellite images are useful for soil inventory and for analysis of soilscapes. Four main factors influence the soil reflectance in remotely sensed images: mineral composition, soil moisture levels, organic matter content and surface soil texture. The above picture is a digital image acquired by the Thematic Mapper sensor on the Landsat
Earth Observation satellite. Orbiting at an altitude of 750 km the Landsat satellite repeats its coverage of the earth every
16 days while the onboard sensors capture an image of about 185 kilometres x 185 kilometres.
This scene shows an area in central The picture on the right is a photograph taken from a special survey
camera onboard an aeroplane flying at approximately
2000 metres. Using such an image and supporting
fieldwork, a trained analyst can map the locations of Humic
Gleysols (dark brown), Luvisols
(bright) and Gleyic Luvisols
(darker than Luvisols) on the image. Artificial
underground drains are visible in the top-right corner of image (GUGiK
|
|
|
Page 36 |
||||
|
|
|
|
|
|
|
Contents Page |
||||