{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282680171251968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.9795/bullgsj.55.1"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"7059092"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/7059092"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I7059092"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/9676685"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/bullgsj/55/1-2/55_1/_pdf"}},{"identifier":{"@type":"NAID","@value":"40006382992"}},{"identifier":{"@type":"NAID","@value":"130004708162"}}],"dc:title":[{"@language":"ja","@value":"関東平野南部における土壌の地球化学的研究 ― 土壌地球化学図の基礎研究(第5報)総括 ―"},{"@language":"en","@value":"Geochemistry of soils from the southern Kanto district, Japan: Preliminary study for the soil geochemical mapping (part 5: Generalization)."},{"@language":"ja-Kana","@value":"カントウ ヘイヤ ナンブ ニ オケル ドジョウ ノ チキュウ カガクテキ ケンキュウ ドジョウ チキュウ カガクズ ノ キソ ケンキュウ ダイ5ホウ ソウカツ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"In order to characterize the geochemical map of soil elements, major and minor elements were determined for Kuroboku soils, brown forest soils and alluvial soils collected in the southern Kanto district, Japan. The effects of biological accumulation on the soil elements are evaluated with the analyses of several plant materials. Compared to the crustal abundance, the plant materials are often enriched in P, Sb, Zn, Cd, Cu, Ca, Pb, Bi, Mn, Sr, K, Mo, As and Sn, but depleted in Al, Ti, Fe,Li, Cs, Tl, Be, Co, Cr, Ni, V, Ga, La, Ce, Th, U, Y and Zr. Most of the elements enriched in plant materials are generally dominant in the uppermost soil layers, reflecting the biological accumulation process. Whereas the elements depleted in the plant materials are clearly lower in the upper soil layers than the deeper one. This may be caused by the diagenetic transportation and the diluting effects by soil water and organic materials which accumulated during soil forming process. It is assumed that the parent material of the studied Kuroboku soils originated from the atomospheric transport materials such as altered tephra, reworked crustal materials with the fine particles of aeolian dust. The brown forest soils are composed mainly of altered basement rocks, and a small amount of the atomospheric transport materials. Both clastic materials derived from basement rocks and the atomospheric transport materials are significant sources of the alluvial soils. Compared to the noncultivated soils, cultivated soils are dominant in K and P through its suppying the manures. There is a clear difference in the chemical composition of the river sediments and the soils. In some samples collected around the highly industrialized areas, recent anthropogenic pollution for heavy metals are recognized. The geochemical mapping according to analyses of the soil itself will be useful for evaluation of recent environmental pollution and estimation of background level concentration of soil elements."},{"@language":"ja","@value":"土壌地球化学図の作成に関する予察的研究の総括として，関東平野南部で新たに採取した土壌柱状・表層試料中の主・微量成分元素を分析し，土壌中元素の地球化学的挙動を総合的に研究した．土壌における元素の生物濃縮は，実際の樹木・草本試料を灰化・分析して評価した．土壌柱状試料における元素濃度の鉛直変化を支配する要因としては，土壌化の影響，生物濃集，土壌母材の起源等が重要である．生物濃縮の影響を受けないAl, Ti, Fe, Li, Cs, Tl,Be, Co, Cr, Ni, V, Ga, La, Ce, Th, U, Y, Zr等は表層部よりも下層部で高濃度を示すが，これは土壌化に伴なう移動と，水分や腐植質物質による希釈効果である．生物濃縮の影響が大きい元素は，P, Sb, Zn, Cd, Cu, Ca, Pb, Bi,Mn, Sr, K, Mo, As, Sn等であり，これら元素の大部分は柱状試料の最表層部で高濃度を示す．Mn, Ca, K, Cu等 は，最表層部で高濃度を示さない場合が多いが，これは生物濃縮の影響よりも土壌化に伴う溶出や水分等による希釈効果が大きいためであろう．黒ボク土の主要母材は，火山噴出物，近傍裸地からの風塵再移動堆積物，広域風成塵等の大気経由物質であり，元素濃度の地域変化は小さい．褐色森林土の母材は，表層地質を構成する岩石等の風化物を主とし，これに若干の大気経由物質が付加されたもので，元素濃度は地質区分毎に異なる．沖積層土壌は，河川由来の砕屑物と大気経由物質の混合物が母材である．土壌地球化学図は，環境汚染の評価と元素濃度のバックグラウンド値を判定するうえで重要な資料である."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001204051083648","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004505706"},{"@type":"NRID","@value":"9000273006370"},{"@type":"NRID","@value":"9000273026986"},{"@type":"NRID","@value":"9000364786927"},{"@type":"NRID","@value":"9000364790139"},{"@type":"NRID","@value":"9000364790316"},{"@type":"NRID","@value":"9000364786860"},{"@type":"NRID","@value":"9000364790187"},{"@type":"NRID","@value":"9000364790202"},{"@type":"NRID","@value":"9000364790256"},{"@type":"NRID","@value":"9000364790391"},{"@type":"NRID","@value":"9000364790278"}],"foaf:name":[{"@language":"ja","@value":"寺島 滋"},{"@language":"en","@value":"Terashima Shigeru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geoscience, GSJ"},{"@language":"ja","@value":"地球科学情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204051686401","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004505708"},{"@type":"NRID","@value":"9000020644045"},{"@type":"NRID","@value":"9000020732856"},{"@type":"NRID","@value":"9000273006371"}],"foaf:name":[{"@language":"ja","@value":"今井 登"},{"@language":"en","@value":"Imai Noboru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geoscience, GSJ"},{"@language":"ja","@value":"地球科学情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751138408704","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30356638"},{"@type":"NRID","@value":"1000030356638"},{"@type":"NRID","@value":"9000285966969"},{"@type":"NRID","@value":"9000254146735"},{"@type":"NRID","@value":"9000403034643"},{"@type":"NRID","@value":"9000258404268"},{"@type":"NRID","@value":"9000002251875"},{"@type":"NRID","@value":"9000000787781"},{"@type":"NRID","@value":"9000392139513"},{"@type":"NRID","@value":"9000399221931"},{"@type":"NRID","@value":"9000002164304"},{"@type":"NRID","@value":"9000398987989"},{"@type":"NRID","@value":"9000283578215"},{"@type":"NRID","@value":"9000000787777"},{"@type":"NRID","@value":"9000254146646"},{"@type":"NRID","@value":"9000254146733"},{"@type":"NRID","@value":"9000257917743"},{"@type":"NRID","@value":"9000414389490"},{"@type":"NRID","@value":"9000398988163"},{"@type":"NRID","@value":"9000390428284"},{"@type":"NRID","@value":"9000376926616"},{"@type":"NRID","@value":"9000254579383"},{"@type":"NRID","@value":"9000254146649"},{"@type":"NRID","@value":"9000370281213"},{"@type":"NRID","@value":"9000254579430"},{"@type":"NRID","@value":"9000405523510"},{"@type":"NRID","@value":"9000283578201"},{"@type":"NRID","@value":"9000410336363"},{"@type":"NRID","@value":"9000398303081"},{"@type":"NRID","@value":"9000243765752"},{"@type":"NRID","@value":"9000258402036"},{"@type":"NRID","@value":"9000414389428"},{"@type":"NRID","@value":"9000392139233"},{"@type":"NRID","@value":"9000273026983"},{"@type":"NRID","@value":"9000257916554"},{"@type":"NRID","@value":"9000283578273"},{"@type":"NRID","@value":"9000392139281"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/a2snow_ohta"}],"foaf:name":[{"@language":"ja","@value":"太田 充恒"},{"@language":"en","@value":"Ohta Atsuyuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geoscience, GSJ"},{"@language":"ja","@value":"地球科学情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680171252098","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000273006373"}],"foaf:name":[{"@language":"ja","@value":"岡井 貴司"},{"@language":"en","@value":"Okai Takashi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geoscience, GSJ"},{"@language":"ja","@value":"地球科学情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204266396416","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004618168"}],"foaf:name":[{"@language":"ja","@value":"御子柴 真澄"},{"@language":"en","@value":"Mikoshiba Masumi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geoscience, GSJ"},{"@language":"ja","@value":"地球科学情報研究部門"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13464272"},{"@type":"LISSN","@value":"13464272"},{"@type":"EISSN","@value":"2186490X"},{"@type":"NDL_BIB_ID","@value":"000000405158"},{"@type":"ISSN","@value":"13464272"},{"@type":"NCID","@value":"AA11587519"}],"prism:publicationName":[{"@language":"en","@value":"BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN"},{"@value":"地質調査研究報告"},{"@language":"en","@value":"Bull. Geol. Surv. Japan"},{"@value":"地調研報"}],"dc:publisher":[{"@language":"en","@value":"National Institute of Advanced Industrial Science and Technology, Geological Survey of Japan"},{"@language":"ja","@value":"国立研究開発法人 産業技術総合研究所 地質調査総合センター"}],"prism:publicationDate":"2004","prism:volume":"55","prism:number":"1-2","prism:startingPage":"1","prism:endingPage":"18"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/7059092"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I7059092"},{"@id":"https://dl.ndl.go.jp/pid/9676685"},{"@id":"https://www.jstage.jst.go.jp/article/bullgsj/55/1-2/55_1/_pdf"}],"availableAt":"2004","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Kuroboku%20soil","dc:title":"Kuroboku soil"},{"@id":"https://cir.nii.ac.jp/all?q=brown%20forest%20soil","dc:title":"brown forest soil"},{"@id":"https://cir.nii.ac.jp/all?q=alluvial%20soil","dc:title":"alluvial soil"},{"@id":"https://cir.nii.ac.jp/all?q=major%20and%20trace%20element","dc:title":"major and trace element"},{"@id":"https://cir.nii.ac.jp/all?q=geochemical%20behavior","dc:title":"geochemical behavior"},{"@id":"https://cir.nii.ac.jp/all?q=geochemical%20map","dc:title":"geochemical map"},{"@id":"https://cir.nii.ac.jp/all?q=southern%20Kanto%20district","dc:title":"southern Kanto district"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011144926981888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The composition of the continental crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568971653120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"DETERMINATION OF MERCURY IN ONE HUNDRED AND EIGHTEEN GEOCHEMICAL REFERENCE SAMPLES BY COLD VAPOR ATOMIC ABSORPTION SPECTROMETRY"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045195176448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The behavior of gold in unaltered island arc tholeiitic rocks from Izu-Oshima, Fuji, and Osoreyama volcanic areas, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519088627072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comments (December 2002)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371351045888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ionesco sous l'œil des barbares"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843822836480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution of the Elements in Some Major Units of the Earth's Crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794950780928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Research Issues"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205196786560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"関東平野における沖積層土壌の化学組成－土壌地球化学図の基礎研究（第2報）－"},{"@language":"en","@value":"Chemical composition of the alluvial soils from the Kanto District, Japan: Preliminary study for the soil geochemical mapping (part 2)."},{"@language":"ja-Kana","@value":"カントウ ヘイヤ ニ オケル チュウセキソウ ドジョウ ノ カガク ソセイ ドジョウ チキュウ カガクズ ノ キソ ケンキュウ ダイ2ホウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206233899776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological investigation on the origin of the black soil, distributed in Japan."},{"@value":"黒土の成因に関する地質学的検討"},{"@language":"ja-Kana","@value":"コクド ノ セイイン ニ カンスル チシツガクテキ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237092096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The present pollution of river-bed sediments and soil in the Watarase-river basin and the Miyata-river basin: The pollution level after abandoned working of the Ashio copper mine and the Hitachi mine"},{"@value":"渡良瀬川流域および宮田川流域の可川堆積物と土壌の汚染の現状―足尾銅山と日立鉱山の閉山後の汚染レベル"},{"@language":"ja-Kana","@value":"ワタラセガワ リュウイキ オヨビ ミヤタガワ リュウイキ ノ カセン タイセキブツ ト ドジョウ ノ オセン ノ ゲンジョウ アシオ ドウザン ヒタチ コウザン ノ ヘイザン 30ネン オヨビ 20ネンゴ ノ オセン レベル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206556756480","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"土壌中元素濃度分布マッピングシステムによる放射性核種の移動性評価(日本土壌肥料学会2005年度大会プログラム)"},{"@language":"en","@value":"Utilization of the Mapping System for the Evaluation of the Mobility of Radionuclides in Soil (Program for 2005 Annual Meeting of Japanese Society of Soil Science and Plant Nutrition)"},{"@value":"土壌中元素濃度分布マッピングシステムによる放射性核種の移動性評価"},{"@language":"ja-Kana","@value":"ドジョウ チュウゲンソ ノウド ブンプ マッピング システム ニ ヨル ホウシャセイカクシュ ノ イドウセイ ヒョウカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679231250304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Multielement analysis of rocks with the use of geological certified reference material by inductively coupled plasma mass spectrometry."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680170843904","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"関東平野の土壌中微量有害元素(As, Sb, Pb, Cr, Mo, Bi, Cd, Tl)の地球化学的研究 －土壌地球化学図の基礎研究(第3報)－"},{"@language":"en","@value":"Geochemistry of toxic trace elements (As, Sb, Pb, Cr, Mo, Bi, Cd, Tl) in the soils from the Kanto District, Japan: Preliminary study for the soil geochemical mapping (part 3)."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680719630976","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"波長分散型蛍光X線分析装置による植物体化学組成分析の試み"},{"@language":"en","@value":"Analysis of plant samples by wavelength dispersive X-ray fluorescence spectrometer"},{"@language":"ja-Kana","@value":"ハチョウ ブンサンガタ ケイコウ Xセン ブンセキ ソウチ ニ ヨル ショクブツタイ カガク ソセイ ブンセキ ノ ココロミ"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2000000146"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I7059092"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.55.1"},{"@type":"CIA","@value":"40006382992"},{"@type":"CIA","@value":"130004708162"}]}