Ontology type: schema:ScholarlyArticle
2019-03
AUTHORSZhuangcai Tian, Xiujun Guo, Luzheng Qiao, Yonggang Jia, Le Yu
ABSTRACTTo define the transformation steps and understand the influence of the breaking process of internal solitary waves (ISWs) on slope sediments, experiments were conducted to study the interactions between continuous ISWs and slopes. Varying slopes were constructed based on the bottom shape and sediment composition of the northern South China Sea. The changes in the suspended sediment concentration (SSC) were then observed during the shoaling and breaking of ISWs on uniform slopes. The results showed that different types of slope sediments were suspended simultaneously at the wave-breaking position when ISW troughs arrived. After 0.5–4 min, the SSC declined slowly. Each suspension process was similar when the ISWs arrived at continuing intervals of 10 min, but the redeposition process varied for different sediments. Clayey silt and fine sand were not restored to the initial concentration in any of the deposition processes. With continued ISWs, this SSC bias increased and a nepheloid layer gradually formed. The sediment resuspension and deposition processes at the splitting deformation position were similar to those at the wave-breaking position; however, the maximum SSC was only one third to one fifth of the former. The capacity of the ISW to suspend sediments was affected by the seabed slope angle, sediment state (shear strength), wave velocity, and sediment type. The results obtained were not consistent with the experimental results (presented in this study) using traditional sediment resuspension criteria. In future research, modified criteria should thus include relevant parameters reflecting the effects of the sediment state and seabed slope angle on stress. More... »
PAGES959-967
http://scigraph.springernature.com/pub.10.1007/s10064-017-1161-x
DOIhttp://dx.doi.org/10.1007/s10064-017-1161-x
DIMENSIONShttps://app.dimensions.ai/details/publication/pub.1092261162
JSON-LD is the canonical representation for SciGraph data.
TIP: You can open this SciGraph record using an external JSON-LD service: JSON-LD Playground Google SDTT
[
{
"@context": "https://springernature.github.io/scigraph/jsonld/sgcontext.json",
"about": [
{
"id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0403",
"inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/",
"name": "Geology",
"type": "DefinedTerm"
},
{
"id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/04",
"inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/",
"name": "Earth Sciences",
"type": "DefinedTerm"
}
],
"author": [
{
"affiliation": {
"alternateName": "Ocean University of China",
"id": "https://www.grid.ac/institutes/grid.4422.0",
"name": [
"College of Environmental Science and Engineering, Ocean University of China, 266100, Qingdao, People\u2019s Republic of China"
],
"type": "Organization"
},
"familyName": "Tian",
"givenName": "Zhuangcai",
"id": "sg:person.012120272403.36",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.012120272403.36"
],
"type": "Person"
},
{
"affiliation": {
"alternateName": "Ocean University of China",
"id": "https://www.grid.ac/institutes/grid.4422.0",
"name": [
"College of Environmental Science and Engineering, Ocean University of China, 266100, Qingdao, People\u2019s Republic of China",
"Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, 266100, Qingdao, People\u2019s Republic of China"
],
"type": "Organization"
},
"familyName": "Guo",
"givenName": "Xiujun",
"id": "sg:person.011233022123.47",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.011233022123.47"
],
"type": "Person"
},
{
"affiliation": {
"alternateName": "Ocean University of China",
"id": "https://www.grid.ac/institutes/grid.4422.0",
"name": [
"College of Environmental Science and Engineering, Ocean University of China, 266100, Qingdao, People\u2019s Republic of China"
],
"type": "Organization"
},
"familyName": "Qiao",
"givenName": "Luzheng",
"id": "sg:person.015106174403.04",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015106174403.04"
],
"type": "Person"
},
{
"affiliation": {
"alternateName": "Ocean University of China",
"id": "https://www.grid.ac/institutes/grid.4422.0",
"name": [
"College of Environmental Science and Engineering, Ocean University of China, 266100, Qingdao, People\u2019s Republic of China",
"Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, 266100, Qingdao, People\u2019s Republic of China"
],
"type": "Organization"
},
"familyName": "Jia",
"givenName": "Yonggang",
"id": "sg:person.013314454402.62",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013314454402.62"
],
"type": "Person"
},
{
"affiliation": {
"alternateName": "Ocean University of China",
"id": "https://www.grid.ac/institutes/grid.4422.0",
"name": [
"College of Environmental Science and Engineering, Ocean University of China, 266100, Qingdao, People\u2019s Republic of China"
],
"type": "Organization"
},
"familyName": "Yu",
"givenName": "Le",
"type": "Person"
}
],
"citation": [
{
"id": "https://doi.org/10.1029/jc093ic10p12317",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1006073209"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.csr.2015.09.022",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1008905100"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.margeo.2010.10.009",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1019509047"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1175/1520-0485(1985)015<1625:tssise>2.0.co;2",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1024278424"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.dsr2.2004.09.016",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1027859569"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.csr.2013.10.019",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1027921095"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/s0380-1330(00)70711-8",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1031732148"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1029/2004jc002394",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1031782114"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1038/srep05937",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1042233367",
"https://doi.org/10.1038/srep05937"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1002/2013jc009360",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1043940654"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.csr.2006.07.022",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1045812980"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1016/j.oceaneng.2005.11.019",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1047246515"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1111/1755-6724.12779",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1049344460"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1029/2007jc004411",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1050668972"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1111/j.1365-3091.1977.tb00136.x",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1051016571"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1029/92jc02955",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1051024039"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1002/2014jc010401",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1052044330"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1017/s0022112085003081",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1053927850"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1017/jfm.2011.432",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1053984836"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1017/jfm.2011.432",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1053984836"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1063/1.3327289",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1057937070"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1109/joe.2004.840839",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1061292697"
],
"type": "CreativeWork"
},
{
"id": "https://doi.org/10.1175/1520-0485(1997)027<1181:srambr>2.0.co;2",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1063422539"
],
"type": "CreativeWork"
}
],
"datePublished": "2019-03",
"datePublishedReg": "2019-03-01",
"description": "To define the transformation steps and understand the influence of the breaking process of internal solitary waves (ISWs) on slope sediments, experiments were conducted to study the interactions between continuous ISWs and slopes. Varying slopes were constructed based on the bottom shape and sediment composition of the northern South China Sea. The changes in the suspended sediment concentration (SSC) were then observed during the shoaling and breaking of ISWs on uniform slopes. The results showed that different types of slope sediments were suspended simultaneously at the wave-breaking position when ISW troughs arrived. After 0.5\u20134 min, the SSC declined slowly. Each suspension process was similar when the ISWs arrived at continuing intervals of 10 min, but the redeposition process varied for different sediments. Clayey silt and fine sand were not restored to the initial concentration in any of the deposition processes. With continued ISWs, this SSC bias increased and a nepheloid layer gradually formed. The sediment resuspension and deposition processes at the splitting deformation position were similar to those at the wave-breaking position; however, the maximum SSC was only one third to one fifth of the former. The capacity of the ISW to suspend sediments was affected by the seabed slope angle, sediment state (shear strength), wave velocity, and sediment type. The results obtained were not consistent with the experimental results (presented in this study) using traditional sediment resuspension criteria. In future research, modified criteria should thus include relevant parameters reflecting the effects of the sediment state and seabed slope angle on stress.",
"genre": "research_article",
"id": "sg:pub.10.1007/s10064-017-1161-x",
"inLanguage": [
"en"
],
"isAccessibleForFree": false,
"isPartOf": [
{
"id": "sg:journal.1136592",
"issn": [
"1435-9529",
"1435-9537"
],
"name": "Bulletin of Engineering Geology and the Environment",
"type": "Periodical"
},
{
"issueNumber": "2",
"type": "PublicationIssue"
},
{
"type": "PublicationVolume",
"volumeNumber": "78"
}
],
"name": "Experimental investigation of slope sediment resuspension characteristics and influencing factors beneath the internal solitary wave-breaking process",
"pagination": "959-967",
"productId": [
{
"name": "readcube_id",
"type": "PropertyValue",
"value": [
"e5b058cfe277e6ae327477834cc26c0ef14730df13ac13828818b7e474e3efa2"
]
},
{
"name": "doi",
"type": "PropertyValue",
"value": [
"10.1007/s10064-017-1161-x"
]
},
{
"name": "dimensions_id",
"type": "PropertyValue",
"value": [
"pub.1092261162"
]
}
],
"sameAs": [
"https://doi.org/10.1007/s10064-017-1161-x",
"https://app.dimensions.ai/details/publication/pub.1092261162"
],
"sdDataset": "articles",
"sdDatePublished": "2019-04-11T12:54",
"sdLicense": "https://scigraph.springernature.com/explorer/license/",
"sdPublisher": {
"name": "Springer Nature - SN SciGraph project",
"type": "Organization"
},
"sdSource": "s3://com-uberresearch-data-dimensions-target-20181106-alternative/cleanup/v134/2549eaecd7973599484d7c17b260dba0a4ecb94b/merge/v9/a6c9fde33151104705d4d7ff012ea9563521a3ce/jats-lookup/v90/0000000364_0000000364/records_72862_00000000.jsonl",
"type": "ScholarlyArticle",
"url": "https://link.springer.com/10.1007%2Fs10064-017-1161-x"
}
]
Download the RDF metadata as: json-ld nt turtle xml License info
JSON-LD is a popular format for linked data which is fully compatible with JSON.
curl -H 'Accept: application/ld+json' 'https://scigraph.springernature.com/pub.10.1007/s10064-017-1161-x'
N-Triples is a line-based linked data format ideal for batch operations.
curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.1007/s10064-017-1161-x'
Turtle is a human-readable linked data format.
curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/s10064-017-1161-x'
RDF/XML is a standard XML format for linked data.
curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/s10064-017-1161-x'
This table displays all metadata directly associated to this object as RDF triples.
156 TRIPLES
21 PREDICATES
49 URIs
19 LITERALS
7 BLANK NODES