Rehabilitation planning in an oilfield in the Monte Austral: mapping sand-sized sediment availability and assessing its effect on microtopography rehabilitation

CIANCIO MATÍAS EZEQUIEL; GUIDA JOHNSON BÁRBARA; ZULETA GUSTAVO ADOLFO

EARTH SURFACE PROCESSES AND LANDFORMS

JOHN WILEY & SONS LTD

Lugar: Londres; Año: 2022

0197-9337

In drylands, the microtopography is formed by mound-shaped dunes of eolian deposition that occurs around shrubs or other vegetation in clumps. These mounds are characteristic of the Monte Austral, which covers 20% of Argentina (approximately 50 million ha), has a strong water deficit and is subjected to land degradation by the oil industry. Considering the biogeomorphological approach, oilfield rehabilitation should begin with regeneration of the mounds as they provide safe sites for vegetation. Since rehabilitation success may be influenced by sand-sized sediment availability, we addressed two objectives: mapping the sediment availability in an oilfield and evaluating its effect on microtopography rehabilitation. We used a Sentinel-2 MSI scene and assessed three approaches to map the sediments: two expressions of the Normalized Difference Sand Index (NDSI) and the Brightness of the Tasseled Cap Transformation (TCB) feature. We validated the three maps using a geomorphological map. Two maps showed the highest agreement with the geomorphological map and errors were associated with the detection of bright lithified or cohesive material not available for sediment transportation. Then, we evaluated the effect of sediments on microtopography rehabilitation. We compared the morphometric traits of mounds (height, maximum and minimum length) located in areas of low and high sediment availability, in both natural and scarified areas. We considered the time since scarification was applied (8-13, 4-8, or less than 4 years ago). The mounds in the natural areas were larger than the mounds in the scarified areas, so complete microtopography rehabilitation is not achieved 13 years after scarification. The mounds in high sediment availability areas were different from the initial condition 4 years after scarification, whereas differences took 8 years to become evident with low sediment availability. Sediment availability must be considered when designing rehabilitation techniques to ensure the success and sustainability of the project. Our results have implications for the development of a biogeomorphological model to guide rehabilitation planning.