Item talk:Q62530
From geokb
{
"USGS Publications Warehouse": { "schema": { "@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Evaluation of landslide monitoring in the Polish Carpathians", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "ofr20111001", "url": "https://pubs.usgs.gov/publication/ofr20111001" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70006265 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/ofr20111001", "url": "https://doi.org/10.3133/ofr20111001" } ], "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Open-File Report" } ], "datePublished": "2011", "dateModified": "2012-02-02", "abstract": "In response to the June 15, 2010 request from the Polish Geological Institute (PGI) to the U.S. Geological Survey (USGS) for assistance and advice regarding real-time landslide monitoring, landslide specialists from the USGS Landslide Hazard Program visited PGI headquarters and field sites in September 2010. During our visit we became familiar with characteristics of landslides in the Polish Carpathians, reviewed PGI monitoring techniques, and assessed needs for monitoring at recently activated landslides. Visits to several landslides that are monitored by PGI (the Just, Ha\u0144czowa, Szymbark, Siercza and \u0141as\u0144ica landslides) revealed that current data collection (monthly GPS and inclinometer surveys, hourly piezometers readings) is generally sufficient for collecting basic information about landslide displacement, depth, and groundwater conditions. Large landslides are typically hydrologically complex, and we would expect such complexity in Carpathian landslides, given the alternating shale and sandstone stratigraphy and complex geologic structures of the flysch bedrock. Consequently groundwater observations could be improved by installing several piezometers that sample the basal shear zone of each landslide being monitored by PGI. These could be supplemented by additional piezometers at shallower depths to help clarify general flow directions and hydraulic gradients. Remedial works at Ha\u0144czowa\nmake the landslide unsuitable for monitoring as part of an early warning\nnetwork. Monitoring there should focus on continued performance of the remedial\nworks.\nOur suggestions for new monitoring at recently activated landslides are summarized in table 1. Displacement\nmonitoring using extensometers and (or) GPS is a high priority at K\u0142odne, \u0141a\u015bnica,\n\u0141azki, and Siedloki. Geomorphologic mapping of active surface features\n(scarps, cracks, shear zones, folds, and thrusts) in sufficient detail to\nreveal the kinematics of each landslide would greatly help in planning\nsubsurface exploration and monitoring. Mapping should take advantage of\nexisting and future airborne lidar data sets of specific areas, where\navailable. Borehole inclinometers and piezometers would complete the basic\nmonitoring package for these landslides. The landslide at K\u0142odne may be\nwell suited for more detailed monitoring for landslide process research,\nalthough research opportunities exist at the other landslides as well. The\nlandslide near Siedloki may be a good candidate for terrestrial laser scanning\n(TLS). Tandem streamflow gages upstream and downstream from the Siedloki\nlandslide, or laser distance meters to monitor advancement of the toe, may be\nneeded to provide warning of stream blockage of Potok Milowski. A real-time\nwarning system specifically for the \u0141azki landslide might be considered due\nto potential concerns about catastrophic movement into Mi\u0119dzybrodzie\nReservoir.\nChallenges associated with the establishment of a complete real-time monitoring and early warning system are\nfar greater than just the technical and logistical aspects of installing remote\nmonitoring systems at a large number of landslides. Long-term maintenance of a\nlandslide monitoring network will involve considerable effort and expense as\nsensors break-down from exposure to weather, landslide movement, and harsh\nunderground environmental conditions.\nOnce PGI\u2019s planned pilot network\nof 10-20 monitored landslides is operating, a period of observation and\nanalysis will be needed to establish appropriate alert levels and criteria for\nissuing alerts and warnings. Simultaneously, discussions with authorities will\nbe needed to develop action plans for responding to landslide notifications and\n(or) warnings. Public resistance to landslide warnings and mandated evacuations\nmay be high given the low historical incidence of fatalities and injuries\nresulting from Carpathian landslides and the small potential for warnings to\nreduce landslide damage to homes and land. Careful weighing of purpose,\nadvantages, and costs of a large-scale monitoring and early warning program is\nneeded early in the planning process and should be revisited regularly\nthroughout pilot and final implementation.\nIn this report, we present a generic plan for monitoring of a hypothetical Carpathian landslide that\nillustrates how our suggestions for each of the specific landslides could be\nimplemented. The plan includes basic pore pressure, displacement, and weather\nmonitoring, along with supplemental monitoring for special conditions at\nspecific landslides. Table 2 summarizes the overall approach and basic\nequipment and software requirements.", "description": "v, 28 p.; Appendix", "publisher": { "@type": "Organization", "name": "U.S. Geological Survey" }, "author": [ { "@type": "Person", "name": "Baum, Rex L. baum@usgs.gov", "givenName": "Rex L.", "familyName": "Baum", "email": "baum@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5337-1970", "url": "https://orcid.org/0000-0001-5337-1970" }, "affiliation": [ { "@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center" } ] }, { "@type": "Person", "name": "Graniczny, Marek", "givenName": "Marek", "familyName": "Graniczny" }, { "@type": "Person", "name": "Perski, Zbigniew", "givenName": "Zbigniew", "familyName": "Perski" }, { "@type": "Person", "name": "Collins, Brian D.", "givenName": "Brian D.", "familyName": "Collins" }, { "@type": "Person", "name": "Raczkowski, Wojciech", "givenName": "Wojciech", "familyName": "Raczkowski" }, { "@type": "Person", "name": "Mrozek, Teresa", "givenName": "Teresa", "familyName": "Mrozek" }, { "@type": "Person", "name": "Nescieruk, Piotr", "givenName": "Piotr", "familyName": "Nescieruk" } ], "funder": [ { "@type": "Organization", "name": "Western Region Geology and Geophysics Science Center", "url": "https://www.usgs.gov/centers/werc" } ] } }, "OpenAlex": { "abstract_inverted_index": { "In": [ 0, 586 ], "response": [ 1 ], "to": [ 2, 14, 73, 179, 263, 363, 372, 394, 456, 485, 504, 510, 518, 546, 550 ], "the": [ 3, 9, 15, 31, 56, 132, 143, 158, 193, 213, 265, 302, 330, 356, 367, 387, 406, 422, 528, 541, 573, 609, 638 ], "June": [ 4 ], "15,": [ 5 ], "2010": [ 6 ], "request": [ 7 ], "from": [ 8, 30, 355, 454, 537 ], "Polish": [ 10, 57 ], "Geological": [ 11, 17 ], "Institute": [ 12 ], "(PGI)": [ 13 ], "U.S.": [ 16 ], "Survey": [ 18 ], "(USGS)": [ 19 ], "for": [ 20, 66, 105, 196, 218, 306, 317, 321, 344, 386, 492, 508, 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"sufficient": [ 104, 261 ], "collecting": [ 106 ], "basic": [ 107, 303, 618, 642 ], "information": [ 108 ], "about": [ 109, 397 ], "displacement,": [ 111, 621 ], "depth,": [ 112 ], "groundwater": [ 114, 147 ], "conditions.": [ 115, 464 ], "Large": [ 116 ], "typically": [ 119 ], "hydrologically": [ 120 ], "complex,": [ 121 ], "would": [ 124, 270, 300 ], "expect": [ 125 ], "such": [ 126 ], "complexity": [ 127 ], "Carpathian": [ 129, 538, 599 ], "landslides,": [ 130 ], "given": [ 131, 527 ], "alternating": [ 133 ], "shale": [ 134 ], "sandstone": [ 136 ], "stratigraphy": [ 137 ], "complex": [ 139 ], "geologic": [ 140 ], "structures": [ 141 ], "flysch": [ 144 ], "bedrock.": [ 145 ], "Consequently": [ 146 ], "observations": [ 148 ], "could": [ 149, 170, 612 ], "be": [ 150, 171, 314, 340, 370, 391, 483, 502, 525, 578, 613 ], "improved": [ 151 ], "installing": [ 153, 428 ], "sample": [ 157 ], "basal": [ 159 ], "shear": [ 160, 255 ], "zone": [ 161 ], "each": [ 163, 268, 607 ], "being": [ 165 ], "PGI.": [ 168 ], "These": [ 169 ], "supplemented": [ 172 ], "additional": [ 174 ], "shallower": [ 177 ], "depths": [ 178 ], "help": [ 180, 272 ], "clarify": [ 181 ], "general": [ 182 ], "flow": [ 183 ], "directions": [ 184 ], "hydraulic": [ 186 ], "gradients.": [ 187 ], "Remedial": [ 188 ], "works": [ 189 ], "Ha\u0144czowa": [ 191 ], "make": [ 192 ], "unsuitable": [ 195 ], "as": [ 198, 333, 451 ], "part": [ 199 ], "an": [ 201 ], "early": [ 202, 414, 566, 571 ], "warning": [ 203, 374, 383, 415, 567 ], "network.": [ 204 ], "Monitoring": [ 205 ], "there": [ 206 ], "should": [ 207, 280, 577 ], "focus": [ 208 ], "on": [ 209 ], "continued": [ 210 ], "performance": [ 211 ], "remedial": [ 214 ], "works.": [ 215 ], "Our": [ 216 ], "suggestions": [ 217, 605 ], "new": [ 219 ], "summarized": [ 226 ], "table": [ 228 ], "1.": [ 229 ], "Displacement": [ 230 ], "using": [ 232 ], "extensometers": [ 233 ], "(or)": [ 235, 514 ], "a": [ 238, 341, 409, 433, 441, 476, 562, 591, 597 ], "high": [ 239, 526 ], "priority": [ 240 ], "K\u0142odne,": [ 242 ], "\u0141a\u015bnica,": [ 243 ], "\u0141azki,": [ 244 ], "Siedloki.": [ 246 ], "Geomorphologic": [ 247 ], "mapping": [ 248 ], "active": [ 250 ], "surface": [ 251 ], "features": [ 252 ], "(scarps,": [ 253 ], "cracks,": [ 254 ], "zones,": [ 256 ], "folds,": [ 257 ], "thrusts)": [ 259 ], "detail": [ 262 ], "reveal": [ 264 ], "kinematics": [ 266 ], "greatly": [ 271 ], "planning": [ 274, 574 ], "subsurface": [ 275 ], "exploration": [ 276 ], "monitoring.": [ 278 ], "Mapping": [ 279 ], "take": [ 281 ], "advantage": [ 282 ], "existing": [ 284 ], "future": [ 286 ], "airborne": [ 287 ], "lidar": [ 288 ], "sets": [ 290 ], "specific": [ 292, 610, 633 ], "areas,": [ 293 ], "where": [ 294 ], "available.": [ 295 ], "Borehole": [ 296 ], "inclinometers": [ 297 ], "complete": [ 301, 410 ], "package": [ 305 ], "these": [ 307 ], "The": [ 309, 335, 615 ], "K\u0142odne": [ 312 ], "may": [ 313, 339, 369, 524 ], "well": [ 315 ], "suited": [ 316 ], "more": [ 318 ], 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Collins", "orcid": "https://orcid.org/0000-0003-4881-5359" }, "institutions": [], "countries": [], "is_corresponding": false, "raw_author_name": "Brian D. Collins", "raw_affiliation_strings": [], "affiliations": [] }, { "author_position": "middle", "author": { "id": "https://openalex.org/A5070062135", "display_name": "Rex L. Baum", "orcid": "https://orcid.org/0000-0001-5337-1970" }, "institutions": [], "countries": [], "is_corresponding": false, "raw_author_name": "Rex L. Baum", "raw_affiliation_strings": [], "affiliations": [] }, { "author_position": "middle", "author": { "id": "https://openalex.org/A5079455172", "display_name": "Teresa Mrozek", "orcid": null }, "institutions": [], "countries": [], "is_corresponding": false, "raw_author_name": "Teresa Mrozek", "raw_affiliation_strings": [], "affiliations": [] }, { "author_position": "middle", "author": { "id": "https://openalex.org/A5023956050", "display_name": "P. 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