Abstract
Remote sensing-based approaches to lithological mapping are traditionally pixel-oriented, with classification performed on either a per-pixel or sub-pixel basis with complete disregard for contextual information about neighbouring pixels. However, intra-class variability due to heterogeneous surface cover (i.e., vegetation and soil) or regional variations in mineralogy and chemical composition can result in the generation of unrealistic, generalised lithological maps that exhibit the “salt-and-pepper” artefact of spurious pixel classifications, as well as poorly defined contacts. In this study, an object-based image analysis (OBIA) approach to lithological mapping is evaluated with respect to its ability to overcome these issues by instead classifying groups of contiguous pixels (i.e., objects). Due to significant vegetation cover in the study area, the OBIA approach incorporates airborne multispectral and LiDAR data to indirectly map lithologies by exploiting associations with both topography and vegetation type. The resulting lithological maps were assessed both in terms of their thematic accuracy and ability to accurately delineate lithological contacts. The OBIA approach is found to be capable of generating maps with an overall accuracy of 73.5% through integrating spectral and topographic input variables. When compared to equivalent per-pixel classifications, the OBIA approach achieved thematic accuracy increases of up to 13.1%, whilst also reducing the “salt-and-pepper” artefact to produce more realistic maps. Furthermore, the OBIA approach was also generally capable of mapping lithological contacts more accurately. The importance of optimising the segmentation stage of the OBIA approach is also highlighted. Overall, this study clearly demonstrates the potential of OBIA for lithological mapping applications, particularly in significantly vegetated and heterogeneous terrain.
Highlights
The use of remotely sensed spectral imagery provides a means of easing both the financial and logistical burden of traditional field-based lithological mapping
The capability of the object-based image analysis (OBIA) approach in discriminating between the lithologies is described in six input datasets, the is in inthe excess of 63%, with an S1–S6 average maximum
It is worth noting that there are on-going attempts to devise more quantitative and automated segmentation parameter selection methods [63,64,65], which are anticipated to help increase the efficiency and optimisation of this process, and produce better results than currently attainable through “trial-and-error” [50]. This first-of-its-kind study evaluates the capability of an OBIA approach for indirectly mapping lithologies in a vegetated landscape using airborne multispectral imagery and airborne LiDAR data
Summary
The use of remotely sensed spectral imagery provides a means of easing both the financial and logistical burden of traditional field-based lithological mapping. This is the case when image classification algorithms are utilised since they provide the capability to automatically identify and map lithologies rapidly over vast areas, whilst reducing the subjectivity associated with visual interpretation of the imagery [1]. An extensive range of classification algorithms has been used in conjunction with multi- and hyperspectral imagery for lithological mapping. Image classifiers employed for lithological mapping purposes have been almost exclusively pixel-based, performing classification on a per-pixel or sub-pixel basis with complete disregard for any contextual information about neighbouring pixels [3].
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