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Research about Montana, South Dakota

Source-linked reports with geographic coverage including Montana, South Dakota.

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Beyond presence mapping: Predicting fractional cover of non-native vegetation in Sentinel-2 imagery using an ensemble of MaxEnt models

Non-native species maps are important tools for understanding and managing biological invasions. We demonstrate a novel approach to extend presence modeling to map fractional cover (FC) of non-native yellow sweet clover Melilotus officinalis in the Northern Great Plains, USA. We used ensembles of MaxEnt models to map FC across landscapes from satellite imagery trained from regional aerial imagery that was trained by local unmanned aerial vehicle (UAV) imagery. Clover cover from field surveys and classified UAV imagery were nearly identical ( n = 22, R 2 = 0.99). Two classified UAV images provided training data to map clover presence with MaxEnt and National Agricultural Imagery Program (NAIP) aerial imagery. We binned cover predictions from NAIP imagery within each Sentinel-2 pixel into eight cover classes to create pure (100%) and FC (20%–95%) training data and modeled each class separately using MaxEnt and Sentinel-2 imagery. We mapped pure clover with one classification threshold and compared its performance to 15 candidate maps that included FC predictions outside pure predictions. Each FC map represented alternative combinations of five MaxEnt thresholds and three approaches to assign cover to pixels with multiple predictions from the FC ensemble. Evaluations of performance with independent datasets revealed maps including FC corresponded to field ( n = 32, R 2 range: 0.39–0.68) and UAV ( n = 20, R 2 range: 0.61–0.84) data better than pure clover maps ( R 2 = 0.15 and 0.31, respectively). Overall, the pure clover map predicted 3.2% cover, whereas the three best performing FC maps predicted 6.6%–8.0% cover. Including FC predictions increased accuracy and cover predictions which can improve ecological understanding of invasions. Our method allows efficient FC mapping for vegetative species discernible in UAV imagery and may be especially useful for mapping rare, irruptive or patchily distributed species with poor representation in field data, which challenges landscape-level mapping.

Montana, South Dakota

Extraction and speciation of arsenic in lacustrine sediments

Arsenic was partially extracted with 4.O M hydrochloric acid, from samples collected at 25-cm intervals in a 350-cm column of sediment at Milltown Reservoir, Montana and from a 60-cm core of sediment collected at the Cheyenne River Embayment of Lake Oahe, South Dakota. The sediment in both reservoirs is highly contaminated with arsenic. The extracted arsenic was separated into As(III) and As(V) on acetate form Dowex 1-X8 ion-exchange resin with 0.12 M HCl eluent. Residual arsenic was sequentially extracted with KClO 3 and HCl. Arsenic was determined by graphite-furnace atomic-absorption spectrometry. The analytical results define oxidized and reduced zones in the sediment columns.

Montana, South Dakota

Tertiary landslides, northwestern South Dakota and Southeastern Montana

Landslide blocks of latest Oligocene or earliest Miocene age are preserved at several localities in northwestern South Dakota and southeastern Montana. These tilted blocks contain Late Cretaceous to late Oligocene rocks and are unconformably overlain by nearly horizontal strata of the Arikaree Formation of Miocene age. Undisturbed rocks of late Oligocene age were completely stripped from the area by pre-Arikaree erosion. More than 100 landslide blocks are preserved in the Slim Buttes, Harding County, South Dakota. Some of the blocks are several miles long, 600 feet wide, and contain a thickness of 300 feet or more of relatively unbroken or unjumbled strata which have been displaced downward as much as 250 feet. The strike of the tilted blocks is about N. 60° W., and the dip of the bedding in the blocks at most places is to the southwest and ranges from a few to more than 60°. Most of the rock in the blocks consists of coarse arkosic sandstone, tuffaceous siltstone, claystone, and thick beds of bentonite of the Chadron and Brule formations of Oligocene age. In a few places, small sections of the underlying Paleocene strata are tilted. The blocks formed along northwest-trendingpre-Arikaree valley walls and escarpments. The major joint system of underlying rocks apparently controlled the orientation of the slides, and the dip of these older rocks facilitated the downward and outward movement of the landslide blocks. The Short Pine Hills, Harding County, South Dakota, and the Long Pine Hills, Carter County, Montana, contain numerous landslide blocks that are similar in orientation and geologic setting to those of the Slim Buttes. In contrast, the Finger Buttes of Carter County, Montana, contain landslide blocks that strike about N. 70° E. and dip to the southeast. This lack of parallelism with blocks of nearby areas is apparently due to the lack of a well-developed joint system in underlying rocks of this area. The presence of the complete sequence of Oligocene rocks in the downdropped blocks indicates that before pre-Arikaree erosion the area was covered by 500 feet or more of beds of the Chadron and Brule formations. These landslide blocks show that the time interval represented by the unconformity at the base of the Arikaree Formation was of relatively short duration.

Montana, South Dakota