Loading…

Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China

Blowouts are an important ground indication of wind-sand activity in the Hulunbuir grassland. They include two basic geomorphologic units, erosion depression and sand deposition, and three typical morphological types: saucer type, trough type, and compound type. In this study, the dynamic changes of...

Full description

Saved in:
Bibliographic Details
Published in:Mathematical problems in engineering 2017-01, Vol.2017 (2017), p.1-17
Main Authors: Yang, Yi, Hasi, Eerdun, Guan, Chao
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923
cites cdi_FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923
container_end_page 17
container_issue 2017
container_start_page 1
container_title Mathematical problems in engineering
container_volume 2017
creator Yang, Yi
Hasi, Eerdun
Guan, Chao
description Blowouts are an important ground indication of wind-sand activity in the Hulunbuir grassland. They include two basic geomorphologic units, erosion depression and sand deposition, and three typical morphological types: saucer type, trough type, and compound type. In this study, the dynamic changes of typical blowouts within the past decade were analyzed via multiperiod high-resolution remote sensing images. RTK was used to repeatedly measure the blowouts to obtain their high-precision 3D terrain data in 2010, 2011, and 2012. Short-term dynamic changes in 3D blowout morphology were carefully analyzed to discover the following. (1) From 2002 to 2012, the depressions of typical blowouts exhibited downwind extension and lateral expansion trends, as they continuously grew in size. Regarding the sand deposition zones, those of the saucer blowout grew continuously, while those of the trough and compound blowouts fluctuated between growth and contraction. (2) The erosion depression of saucer blowouts eroded downward and spread horizontally; that of trough blowouts first accumulated then eroded but also spread horizontally. The erosion depression of compound blowouts exhibited horizontal spreading accompanied with bottom accumulation. The sand deposition zones of all three types of blowouts exhibited decreasing length with increasing width and height.
doi_str_mv 10.1155/2017/9206963
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1904220616</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>4321383967</sourcerecordid><originalsourceid>FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923</originalsourceid><addsrcrecordid>eNqF0M9LwzAUB_AiCur05lkCXgRXl5c0aeNN508YCE7BW0nTVCNdMpuGsf_ejA4EL17y4_HhveSbJCeALwEYmxAM-UQQzAWnO8kBME5TBlm-G8-YZCkQ-r6fHHr_hTEBBsVBYm_XVi6MQtNPaT-0R65Br-ulUbJFN61budB7dCO9rpGz6NF8fKYv2rs29Cbeb2Uvr9A1mkaA5n2o18hEFdpgq2A6NJc2lmZxHccBxsqjZK-RrdfH232UvN3fvU4f09nzw9P0epYqKmifVkoJVggMBLOCEKIaBrympGgIZAJyoELUsS4rXLOGas0bygHyItOsUoLQUXI-9F127jto35cL45VuW2m1C74EgTMSgwIe6dkf-uVCZ-PrSigKCjwr8k3D8aBU57zvdFMuO7OQ3boEXG7CLzfhl9vwI78YePx0LVfmP306aB2NbuSvBkE4zekP17eKqA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1883164872</pqid></control><display><type>article</type><title>Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China</title><source>Wiley Online Library Open Access</source><source>Publicly Available Content Database</source><creator>Yang, Yi ; Hasi, Eerdun ; Guan, Chao</creator><contributor>Bagan, Hasi</contributor><creatorcontrib>Yang, Yi ; Hasi, Eerdun ; Guan, Chao ; Bagan, Hasi</creatorcontrib><description>Blowouts are an important ground indication of wind-sand activity in the Hulunbuir grassland. They include two basic geomorphologic units, erosion depression and sand deposition, and three typical morphological types: saucer type, trough type, and compound type. In this study, the dynamic changes of typical blowouts within the past decade were analyzed via multiperiod high-resolution remote sensing images. RTK was used to repeatedly measure the blowouts to obtain their high-precision 3D terrain data in 2010, 2011, and 2012. Short-term dynamic changes in 3D blowout morphology were carefully analyzed to discover the following. (1) From 2002 to 2012, the depressions of typical blowouts exhibited downwind extension and lateral expansion trends, as they continuously grew in size. Regarding the sand deposition zones, those of the saucer blowout grew continuously, while those of the trough and compound blowouts fluctuated between growth and contraction. (2) The erosion depression of saucer blowouts eroded downward and spread horizontally; that of trough blowouts first accumulated then eroded but also spread horizontally. The erosion depression of compound blowouts exhibited horizontal spreading accompanied with bottom accumulation. The sand deposition zones of all three types of blowouts exhibited decreasing length with increasing width and height.</description><identifier>ISSN: 1024-123X</identifier><identifier>EISSN: 1563-5147</identifier><identifier>DOI: 10.1155/2017/9206963</identifier><language>eng</language><publisher>Cairo, Egypt: Hindawi Publishing Corporation</publisher><subject>Blowouts ; Deposition ; Depression ; Dynamic tests ; Dynamics ; Erosion ; Geomorphology ; Grasslands ; High resolution ; Image resolution ; Morphology ; Remote sensing ; Sand ; Soil erosion ; Vegetation</subject><ispartof>Mathematical problems in engineering, 2017-01, Vol.2017 (2017), p.1-17</ispartof><rights>Copyright © 2017 Yi Yang et al.</rights><rights>Copyright © 2017 Yi Yang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923</citedby><cites>FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923</cites><orcidid>0000-0003-1365-9480</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/1883164872/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/1883164872?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,25753,27924,27925,37012,37013,44590,74998</link.rule.ids></links><search><contributor>Bagan, Hasi</contributor><creatorcontrib>Yang, Yi</creatorcontrib><creatorcontrib>Hasi, Eerdun</creatorcontrib><creatorcontrib>Guan, Chao</creatorcontrib><title>Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China</title><title>Mathematical problems in engineering</title><description>Blowouts are an important ground indication of wind-sand activity in the Hulunbuir grassland. They include two basic geomorphologic units, erosion depression and sand deposition, and three typical morphological types: saucer type, trough type, and compound type. In this study, the dynamic changes of typical blowouts within the past decade were analyzed via multiperiod high-resolution remote sensing images. RTK was used to repeatedly measure the blowouts to obtain their high-precision 3D terrain data in 2010, 2011, and 2012. Short-term dynamic changes in 3D blowout morphology were carefully analyzed to discover the following. (1) From 2002 to 2012, the depressions of typical blowouts exhibited downwind extension and lateral expansion trends, as they continuously grew in size. Regarding the sand deposition zones, those of the saucer blowout grew continuously, while those of the trough and compound blowouts fluctuated between growth and contraction. (2) The erosion depression of saucer blowouts eroded downward and spread horizontally; that of trough blowouts first accumulated then eroded but also spread horizontally. The erosion depression of compound blowouts exhibited horizontal spreading accompanied with bottom accumulation. The sand deposition zones of all three types of blowouts exhibited decreasing length with increasing width and height.</description><subject>Blowouts</subject><subject>Deposition</subject><subject>Depression</subject><subject>Dynamic tests</subject><subject>Dynamics</subject><subject>Erosion</subject><subject>Geomorphology</subject><subject>Grasslands</subject><subject>High resolution</subject><subject>Image resolution</subject><subject>Morphology</subject><subject>Remote sensing</subject><subject>Sand</subject><subject>Soil erosion</subject><subject>Vegetation</subject><issn>1024-123X</issn><issn>1563-5147</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><recordid>eNqF0M9LwzAUB_AiCur05lkCXgRXl5c0aeNN508YCE7BW0nTVCNdMpuGsf_ejA4EL17y4_HhveSbJCeALwEYmxAM-UQQzAWnO8kBME5TBlm-G8-YZCkQ-r6fHHr_hTEBBsVBYm_XVi6MQtNPaT-0R65Br-ulUbJFN61budB7dCO9rpGz6NF8fKYv2rs29Cbeb2Uvr9A1mkaA5n2o18hEFdpgq2A6NJc2lmZxHccBxsqjZK-RrdfH232UvN3fvU4f09nzw9P0epYqKmifVkoJVggMBLOCEKIaBrympGgIZAJyoELUsS4rXLOGas0bygHyItOsUoLQUXI-9F127jto35cL45VuW2m1C74EgTMSgwIe6dkf-uVCZ-PrSigKCjwr8k3D8aBU57zvdFMuO7OQ3boEXG7CLzfhl9vwI78YePx0LVfmP306aB2NbuSvBkE4zekP17eKqA</recordid><startdate>20170101</startdate><enddate>20170101</enddate><creator>Yang, Yi</creator><creator>Hasi, Eerdun</creator><creator>Guan, Chao</creator><general>Hindawi Publishing Corporation</general><general>Hindawi</general><general>Hindawi Limited</general><scope>ADJCN</scope><scope>AHFXO</scope><scope>RHU</scope><scope>RHW</scope><scope>RHX</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>CWDGH</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>JQ2</scope><scope>K7-</scope><scope>KR7</scope><scope>L6V</scope><scope>M7S</scope><scope>P5Z</scope><scope>P62</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><orcidid>https://orcid.org/0000-0003-1365-9480</orcidid></search><sort><creationdate>20170101</creationdate><title>Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China</title><author>Yang, Yi ; Hasi, Eerdun ; Guan, Chao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Blowouts</topic><topic>Deposition</topic><topic>Depression</topic><topic>Dynamic tests</topic><topic>Dynamics</topic><topic>Erosion</topic><topic>Geomorphology</topic><topic>Grasslands</topic><topic>High resolution</topic><topic>Image resolution</topic><topic>Morphology</topic><topic>Remote sensing</topic><topic>Sand</topic><topic>Soil erosion</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Yi</creatorcontrib><creatorcontrib>Hasi, Eerdun</creatorcontrib><creatorcontrib>Guan, Chao</creatorcontrib><collection>الدوريات العلمية والإحصائية - e-Marefa Academic and Statistical Periodicals</collection><collection>معرفة - المحتوى العربي الأكاديمي المتكامل - e-Marefa Academic Complete</collection><collection>Hindawi Publishing Complete</collection><collection>Hindawi Publishing Subscription Journals</collection><collection>Hindawi Publishing Open Access</collection><collection>CrossRef</collection><collection>Mechanical &amp; Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies &amp; Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>Middle East &amp; Africa Database</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Computer Science Collection</collection><collection>Computer Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>Engineering Database</collection><collection>Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><jtitle>Mathematical problems in engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yang, Yi</au><au>Hasi, Eerdun</au><au>Guan, Chao</au><au>Bagan, Hasi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China</atitle><jtitle>Mathematical problems in engineering</jtitle><date>2017-01-01</date><risdate>2017</risdate><volume>2017</volume><issue>2017</issue><spage>1</spage><epage>17</epage><pages>1-17</pages><issn>1024-123X</issn><eissn>1563-5147</eissn><abstract>Blowouts are an important ground indication of wind-sand activity in the Hulunbuir grassland. They include two basic geomorphologic units, erosion depression and sand deposition, and three typical morphological types: saucer type, trough type, and compound type. In this study, the dynamic changes of typical blowouts within the past decade were analyzed via multiperiod high-resolution remote sensing images. RTK was used to repeatedly measure the blowouts to obtain their high-precision 3D terrain data in 2010, 2011, and 2012. Short-term dynamic changes in 3D blowout morphology were carefully analyzed to discover the following. (1) From 2002 to 2012, the depressions of typical blowouts exhibited downwind extension and lateral expansion trends, as they continuously grew in size. Regarding the sand deposition zones, those of the saucer blowout grew continuously, while those of the trough and compound blowouts fluctuated between growth and contraction. (2) The erosion depression of saucer blowouts eroded downward and spread horizontally; that of trough blowouts first accumulated then eroded but also spread horizontally. The erosion depression of compound blowouts exhibited horizontal spreading accompanied with bottom accumulation. The sand deposition zones of all three types of blowouts exhibited decreasing length with increasing width and height.</abstract><cop>Cairo, Egypt</cop><pub>Hindawi Publishing Corporation</pub><doi>10.1155/2017/9206963</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0003-1365-9480</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1024-123X
ispartof Mathematical problems in engineering, 2017-01, Vol.2017 (2017), p.1-17
issn 1024-123X
1563-5147
language eng
recordid cdi_proquest_miscellaneous_1904220616
source Wiley Online Library Open Access; Publicly Available Content Database
subjects Blowouts
Deposition
Depression
Dynamic tests
Dynamics
Erosion
Geomorphology
Grasslands
High resolution
Image resolution
Morphology
Remote sensing
Sand
Soil erosion
Vegetation
title Dynamic Changes of Typical Blowouts Based on High-Resolution Data: A Case Study in Hulunbuir Sandy Land, China
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T01%3A10%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Dynamic%20Changes%20of%20Typical%20Blowouts%20Based%20on%20High-Resolution%20Data:%20A%20Case%20Study%20in%20Hulunbuir%20Sandy%20Land,%20China&rft.jtitle=Mathematical%20problems%20in%20engineering&rft.au=Yang,%20Yi&rft.date=2017-01-01&rft.volume=2017&rft.issue=2017&rft.spage=1&rft.epage=17&rft.pages=1-17&rft.issn=1024-123X&rft.eissn=1563-5147&rft_id=info:doi/10.1155/2017/9206963&rft_dat=%3Cproquest_cross%3E4321383967%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c393t-bcc9589012058222cf516d328f2149171399d222ab0d5f3ee6f3611784e5bc923%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1883164872&rft_id=info:pmid/&rfr_iscdi=true