Abstract
A total of 66,894 landslides were observed in North Dakota. The characteristics of these landslide locations were compared with the properties of areas without landslides to assess the factors that may be contributing to the landslides. Specifically, 68,395 control point locations randomly distributed across the state were selected for these comparisons. All the landslides for this study were found in areas with slopes less than 64°, with the majority of the failures occurring on slopes with inclinations between 9° and 14°. The largest fraction of the landslides occurred in the Sentinel Butte Formation (34,063 or 51% of the total), followed by Bullion Creek (8695 or 13% of the total) and river sediment of the Oahe Formation (6421 or 9.6% of the total). In the t tests, all of the surficial geologic formations had statistically significant differences between the landslides and control points. The t test for the slope inclination indicated statistically significant differences with a p-value less than 0.001 and a huge effect size between the landslide and control points. The sodium adsorption ratio and total dissolved solids were also found to be statistically significant from the t test results. Pearson’s correlation matrix showed a negative correlation between the amount of rainfall and various measures of the salt concentrations at the landslide locations, pointing to the reductions in shear strength and slope stability that might result as pore fluid salinity is leached.
Data availability
Some or all data, models or codes that support the findings of this article are avialable from the corresponding author upon reasonable request.
References
ACIS (2020) NOAA: regional climate centers. Appl Clim Info Sys.http://scacis.rcc-acis.org/
Anderson FJ, Maike CA (2017) Drones rising from the prairie: geological applications of unmanned aerial systems. GeoNews 44(2):8–14. https://www.dmr.nd.gov/ndgs/documents/newsletter/2017Summer/Drones%20Rising%20from%20the%20Prairie.pdf
Bluemle JP (1983) Geologic and topographic bedrock map of North Dakota, North Dakota geological survey. It can be found at: https://www.dmr.nd.gov/ndgs/documents/Publication_List/pdf/MisMaps/MM-25.pdf
Bluemle J, Biek B (2007) No ordinary plain-North Dakota’s physiography and landforms. N Dakota Geol Surv. https://www.dmr.nd.gov/ndgs/ndnotes/ndn1.asp
City-Data (2020) North Dakota location, size and extent. North Dakota. http://www.city-data.com/states/North-Dakota-Location-size-and-extent.html
Clayton L (1980a) Geologic Map of North Dakota. US Geol Surv
Clayton L (1980b) Explanatory text to accompany the geologic map of North Dakota. North Dakota Geological Survey, Grand Forks
Corwin DL, Yemoto K (2017) Salinity: electrical conductivity and total dissolved solids. Soil Science Society of America 84(5):1442–1461
Davis JG, Waskom RM, Bauder JA (2012) Managing sodic soils. Colorado State University, Fort Collins, CO
Day RW (1993) Surficial slope failure: a case study. J Perform Constr Facil 7(4):264–269
Derby NE, Wick A, Casey FXM (2014) Spatially variable soil salinity, chemistry, and physical properties affect soil health. Soil Sci Soc Am Int Annual Meeting 2–5. Long Beach, CA
Dunaway D, Swanson SR, Wendel J, Clary W (1994) The effect of herbaceous plant communities and soil textures on particle erosion of alluvial streambanks. Geomorphology 9(1):47–56
EMDAT (2020) The International Disaster Database. Centr Res Epidemiol Disasters. https://www.emdat.be
Enz JW (2003) North Dakota topographic, climatic, and agricultural overview. North Dakota State University. https://www.ndsu.edu/fileadmin/ndsco/documents/ndclimate.pdf
Ghestem M, Veylon G, Bernard A, Vanel Q, Stokes A (2014) Influence of plant root system morphology and architectural traits on soil shear resistance. Plant Soil 377(1):43–61
Gill JR, Cobban WA (1965) Stratigraphy of the Pierre Shale, Valley City and Pembina Mountain Areas, North Dakota. US Government Printing Office, Washington
Godt JW, Coe JA, Baum RL, Highlighd LM, Keaton JR, Roth RJ (2012) “Prototype landslide hazard maps of the conterminous United States. Protecting Society through Improved Understanding, Landslides and Engineering Slopes, pp 245–250
Goulet-Pelletier J-C, Cousineau D (2018) A review of effect sizes and their confidence intervals, Part I: The Cohen’s d family. The Quantitative Methods for Psychology 14(4):242–265
Highland L, Bobrowsky PT (2008) The landslide handbook: a guide to understanding landslides. US Geological Survey, Reston, Virginia
Jacob AF (1976) Geology of the Upper Part of the Fort Union Group (Paleocene), Williston Basin, with Reference to Uranium. North Dakota Geological Survey, Grand Forks
Keller LP, McCarthy GJ, Richardson JL (1986) Mineralogy and stability of soil evaporates in North Dakota. Soil Sci Soc Am J 50:1069–1071
Kline VH (1942) Stratigraphy of North Dakota. AAPG Bull 26(3):336–379
Kodikara J, Barbour SL, Fredlund DG (1999) Changes in clay structure and behaviour due to wetting and drying. In Proceedings 8th Australia New Zealand conference on geomechanics: consolidating knowledge (Vol. 179). Barton, ACT: Australian Geomechanics Society
Lasdon LS, Waren AD, Jain A, Ratner M (1978) Design and Testing of a Generalized Reduced Gradient Code for Nonlinear Programming. ACM Trans Math Softw 4(1):34–50
Mirus BB, Jones ES, Baum RL, Godt JW, Slaughter S, Crawford MM, Lancaster J, Stanley T, Kirschbaum DB, Burns WJ, Schmitt RG, Lindsey KO, McCoy KM (2020) Landslides across the USA: occurrence, susceptibility, and data limitations. Landslides 17:2271–2285. https://doi.org/10.1007/s10346-020-01424-4
Mitchell JK, Soga K (2005) Fundamentals of soil behavior, 3rd edn. John Wiley & Sons Inc, Wiley, New York
Moxness LD (2019) Twenty thousand slides and counting: recent advances in digital imagery expedite landslides mapping in North Dakota. GeoNews 17–19. https://www.dmr.nd.gov/ndgs/documents/newsletter/2019Winter/Twenty_Thousand_Slides_and_Counting.pdf
Moxness LD (2022) The first statewide landslide dataset: NDGS completes initial landslide mapping for North Dakota. GeoNews 12–15. https://www.dmr.nd.gov/ndgs/documents/newsletter/2022Winter/The_First_Statewide_Landslide_Dataset.pdf
Muñoz Sabater J (2019) ERA5-Land monthly averaged data from 1981 to present. Copernicus Climate Change Service (C3S) Climate Data Store (CDS). https://doi.org/10.24381/cds.68d2bb30
Murphy EC (2017) Landslides in North Dakota. GeoNews 44(1):1–5
Murphy EC, Nordeng SH, Juenker BJ, Hoganson JW (2009) North Dakota Stratigraphic Column: North Dakota Geological Survey Miscellaneous Series 91. N Dakota Geol Surv
ND (2020) Climate. Game and Fish. https://gf.nd.gov/wildlife/habitats/climate#:~:text=Annual%20precipitation%20ranges%20from%2013,to%204%20inches%20of%20rain
ND (2021) North Dakota plants and habitats overview. North Dakota Game and Fish Department. https://gf.nd.gov/wildlife/habitats/vegetation
NLCD (2016) National Land Cover Database 2016. Multi-Resolution Land Characteristics Consortium. https://www.mrlc.gov/data/legends/national-land-cover-database-2016-nlcd2016-legend#:~:text=Grassland%2FHerbaceous%2D%20areas%20dominated%20by,can%20be%20utilized%20for%20grazing
NOAA (2017) Climate of North Dakota. National Oceanic and Atmospheric Administration. https://web.archive.org/web/20070926010149/http://www5.ncdc.noaa.gov/climatenormals/clim60/states/Clim_ND_01.pdf
NOAA (2020) National Weather Service: national snowfall analysis. National Oceanic and Atmospheric Administration. https://www.nohrsc.noaa.gov/snowfall_v2/index.html?season=2009-2010&date=2011060912&version=3&format=.tif
Parker GG, Higgins CG, Wood WW (1990) Piping and pseudokarst in drylands. Geol Soc Am Spec Pap 252:77–110
Pearson KE (2020) Basics of salinity and sodicity effects on soil physical properties. Montana State University. https://waterquality.montana.edu/energy/cbm/background/soil-prop.html
Radbrunch-Hall DH, Colton RB, Davies WE, Luchhitta I, Skipp BA, Vanes DJ (1982) Landslide overview map of the conterminous United States. U.S. Geol Surv Prof Paper 1183
Ratner B (2009) The correlation coefficient: its values range between + 1/− 1, or do they? J Target Meas Anal Mark 17(2):139–142
Ritchie H, Roser M (2014) Natural disasters. Our World in Data. https://ourworldindata.org/natural-disasters
Sawilowsky SS (2009) New effect size rules of thumb. J Mod Appl Stat Methods 8(2):597–599
Schaefer VR, Birchmier MA (2013) Mechanisms of strength loss during wetting and drying of Pierre Shale. Proc 18th Int Conf Soil Mech Geotech Eng 1183–1186
Schuster RL (1978) Introduction, Chapter 1. Trans Res Board Special Rep 176:1–10
Tiwari B, Ajmera B (2015) Reduction in fully softened shear strength of natural clays with NaCl leaching and its effect on slope stability. Journal of Geotechnical and Geoenvironmental Engineering 141(1):04014086
Tiwari B, Tuladhar GR, Marui H (2005) Variation in residual shear strength of the soil with the salinity of pore fluid. Journal of Geotechnical and Geoenvironmental Engineering 131(12):1445–1456
USDA (2013) National soil survey handbook. Title 430-VI
USDA (2020) Web soil survey. Nat Resour Conserv Serv. https://websoilsurvey.nrcs.usda.gov/
USGS (2016) NLCD land cover (CONUS). MRLC. https://www.mrlc.gov/data?f%5B0%5D=category%3ALand%20Cover
USGS (2019) USGS National Elevation Dataset (NED). ND State Water Commission. https://catalog.data.gov/dataset/usgs-national-elevation-dataset-ned
Vlotman WF, Smedema LK, Rycroft DW (2020) Modern land drainage: planning, design and management of agricultural drainage systems. CRC Press
Wallick BP (1984) Sedimentology of the bullion creek and sentinel butte formations (Paleocene) in a part of southern McKenzie County, North Dakota. Theses and Dissertations 311
Warrence NJ, Bauder JW, Pearson KE (2002) Basics of salinity and sodicity effects on soil physical properties. Department of Land Resources and Environmental Sciences, Montana State University-Bozeman, MT, 129:1–29
Zhang C-B, Chen L-H, Liu Y-P, Ji X-D, Liu X-P (2010) Triaxial compression test of soil–root composites to evaluate influence of roots on soil shear strength. Ecol Eng 36(1):19–26
Funding
The authors appreciate the financial support provided by the Geopier Foundation Company Midwest Scholarship, the Braun Intertec Corporation, the Department of Civil, Construction, and Environmental Engineering at Iowa State University, and the Department of Civil and Environmental Engineering (now, Civil, Construction, and Environmental Engineering) at North Dakota State University. Braun Intertac Corporation is also acknowledged for its support in conducting field investigations of the several landslide locations described in this study.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
The authors certify that they have no affiliations with or involvement in any organizations or entities with any financial or non-financial interest in the subject matter or materials discussed in this paper.
Rights and permissions
About this article
Cite this article
Shafer, B., Ajmera, B., Upadhaya, K.R. et al. Assessment of factors leading to the failure of slopes in North Dakota. Landslides 21, 1109–1128 (2024). https://doi.org/10.1007/s10346-024-02211-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10346-024-02211-1