The color reflectance of marine-terrigenous deposits in LZ908 borehole in south coastal plain of the Laizhou Bay
Color measuring is characterized by high resolution,high efficiency,and low cost. The application becomes increasingly common for tracing sediment sources and climate variation. Borehole LZ908 in the south coastal plain of the Laizhou Bay in northeast China,was used,of which the top 54 m containing...
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| Veröffentlicht in: | Acta oceanologica Sinica 2011-07, Vol.30 (4), p.53-59 |
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| creator | Zhao, Na Xu, Xingyong Yu, Hongjun Yao, Jing Su, Qiao Peng, Shuzhen |
| description | Color measuring is characterized by high resolution,high efficiency,and low cost. The application becomes increasingly common for tracing sediment sources and climate variation. Borehole LZ908 in the south coastal plain of the Laizhou Bay in northeast China,was used,of which the top 54 m containing all marine facies was focused,to test the feasibility of colorimetry as a climate indi-cator using visible light reflectance spectra and L＊a＊b＊measurement results. The results show a good correction between lightness and calcium carbonate content in marine-terrigenous deposits;therefore,these deposits can be used as a proxy to study climate changes. Factor-analysis on the first derivative values of the raw visible light reflectance spectra produced three principal factors corresponding to goethite,organic matter,and hematite. Down hole variations in the three fac-tor scores,lightness,calcium carbonate content,and grain size were quite consistent. Moreover,high lightness and low factor scores in goethite,hematite,and organics indicated glacial regression deposits,while low lightness and high factor scores in goethite,hematite,and organics indicated interglacial transgression deposits. |
| doi_str_mv | 10.1007/s13131-011-0133-4 |
| format | Article |
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The application becomes increasingly common for tracing sediment sources and climate variation. Borehole LZ908 in the south coastal plain of the Laizhou Bay in northeast China,was used,of which the top 54 m containing all marine facies was focused,to test the feasibility of colorimetry as a climate indi-cator using visible light reflectance spectra and L＊a＊b＊measurement results. The results show a good correction between lightness and calcium carbonate content in marine-terrigenous deposits;therefore,these deposits can be used as a proxy to study climate changes. Factor-analysis on the first derivative values of the raw visible light reflectance spectra produced three principal factors corresponding to goethite,organic matter,and hematite. Down hole variations in the three fac-tor scores,lightness,calcium carbonate content,and grain size were quite consistent. Moreover,high lightness and low factor scores in goethite,hematite,and organics indicated glacial regression deposits,while low lightness and high factor scores in goethite,hematite,and organics indicated interglacial transgression deposits.</description><identifier>ISSN: 0253-505X</identifier><identifier>EISSN: 1869-1099</identifier><identifier>DOI: 10.1007/s13131-011-0133-4</identifier><language>eng</language><publisher>Heidelberg: The Chinese Society of Oceanography</publisher><subject>Boreholes ; Calcium ; Calcium carbonate ; Calcium carbonates ; Carbonates ; Climate change ; Climate studies ; Climatology ; Coastal plains ; Color ; Colorimetry ; Deposits ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Engineering Fluid Dynamics ; Environmental Chemistry ; Goethite ; Grain size ; Haematite ; Hematite ; Interglacial periods ; Marine ; Marine & Freshwater Sciences ; Oceanography ; Organic matter ; Reflectance ; Sediment sources ; Sedimentary facies ; Sediments ; Spectra ; Terrigenous sediments ; 气候变化 ; 沿海平原 ; 海洋 ; 碳酸钙含量 ; 莱州湾 ; 钻孔 ; 陆相沉积 ; 颜色反射率</subject><ispartof>Acta oceanologica Sinica, 2011-07, Vol.30 (4), p.53-59</ispartof><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2011</rights><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2011.</rights><rights>Copyright © Wanfang Data Co. 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Sin</addtitle><addtitle>Acta Oceanologica Sinica</addtitle><description>Color measuring is characterized by high resolution,high efficiency,and low cost. The application becomes increasingly common for tracing sediment sources and climate variation. Borehole LZ908 in the south coastal plain of the Laizhou Bay in northeast China,was used,of which the top 54 m containing all marine facies was focused,to test the feasibility of colorimetry as a climate indi-cator using visible light reflectance spectra and L＊a＊b＊measurement results. The results show a good correction between lightness and calcium carbonate content in marine-terrigenous deposits;therefore,these deposits can be used as a proxy to study climate changes. Factor-analysis on the first derivative values of the raw visible light reflectance spectra produced three principal factors corresponding to goethite,organic matter,and hematite. Down hole variations in the three fac-tor scores,lightness,calcium carbonate content,and grain size were quite consistent. Moreover,high lightness and low factor scores in goethite,hematite,and organics indicated glacial regression deposits,while low lightness and high factor scores in goethite,hematite,and organics indicated interglacial transgression deposits.</description><subject>Boreholes</subject><subject>Calcium</subject><subject>Calcium carbonate</subject><subject>Calcium carbonates</subject><subject>Carbonates</subject><subject>Climate change</subject><subject>Climate studies</subject><subject>Climatology</subject><subject>Coastal plains</subject><subject>Color</subject><subject>Colorimetry</subject><subject>Deposits</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Engineering Fluid Dynamics</subject><subject>Environmental Chemistry</subject><subject>Goethite</subject><subject>Grain size</subject><subject>Haematite</subject><subject>Hematite</subject><subject>Interglacial periods</subject><subject>Marine</subject><subject>Marine & Freshwater Sciences</subject><subject>Oceanography</subject><subject>Organic matter</subject><subject>Reflectance</subject><subject>Sediment sources</subject><subject>Sedimentary facies</subject><subject>Sediments</subject><subject>Spectra</subject><subject>Terrigenous 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香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Acta oceanologica Sinica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhao, Na</au><au>Xu, Xingyong</au><au>Yu, Hongjun</au><au>Yao, Jing</au><au>Su, Qiao</au><au>Peng, Shuzhen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The color reflectance of marine-terrigenous deposits in LZ908 borehole in south coastal plain of the Laizhou Bay</atitle><jtitle>Acta oceanologica Sinica</jtitle><stitle>Acta Oceanol. Sin</stitle><addtitle>Acta Oceanologica Sinica</addtitle><date>2011-07-01</date><risdate>2011</risdate><volume>30</volume><issue>4</issue><spage>53</spage><epage>59</epage><pages>53-59</pages><issn>0253-505X</issn><eissn>1869-1099</eissn><abstract>Color measuring is characterized by high resolution,high efficiency,and low cost. The application becomes increasingly common for tracing sediment sources and climate variation. Borehole LZ908 in the south coastal plain of the Laizhou Bay in northeast China,was used,of which the top 54 m containing all marine facies was focused,to test the feasibility of colorimetry as a climate indi-cator using visible light reflectance spectra and L＊a＊b＊measurement results. The results show a good correction between lightness and calcium carbonate content in marine-terrigenous deposits;therefore,these deposits can be used as a proxy to study climate changes. Factor-analysis on the first derivative values of the raw visible light reflectance spectra produced three principal factors corresponding to goethite,organic matter,and hematite. Down hole variations in the three fac-tor scores,lightness,calcium carbonate content,and grain size were quite consistent. Moreover,high lightness and low factor scores in goethite,hematite,and organics indicated glacial regression deposits,while low lightness and high factor scores in goethite,hematite,and organics indicated interglacial transgression deposits.</abstract><cop>Heidelberg</cop><pub>The Chinese Society of Oceanography</pub><doi>10.1007/s13131-011-0133-4</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0253-505X |
| ispartof | Acta oceanologica Sinica, 2011-07, Vol.30 (4), p.53-59 |
| issn | 0253-505X 1869-1099 |
| language | eng |
| recordid | cdi_wanfang_journals_hyxb_e201104006 |
| source | Springer Nature - Complete Springer Journals; ProQuest Central UK/Ireland; Alma/SFX Local Collection; ProQuest Central |
| subjects | Boreholes Calcium Calcium carbonate Calcium carbonates Carbonates Climate change Climate studies Climatology Coastal plains Color Colorimetry Deposits Earth and Environmental Science Earth Sciences Ecology Engineering Fluid Dynamics Environmental Chemistry Goethite Grain size Haematite Hematite Interglacial periods Marine Marine & Freshwater Sciences Oceanography Organic matter Reflectance Sediment sources Sedimentary facies Sediments Spectra Terrigenous sediments 气候变化 沿海平原 海洋 碳酸钙含量 莱州湾 钻孔 陆相沉积 颜色反射率 |
| title | The color reflectance of marine-terrigenous deposits in LZ908 borehole in south coastal plain of the Laizhou Bay |
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