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Dynamic changes of soil organic carbon under different land use type in Sanjiang Plain

https://chikyu.repo.nii.ac.jp/records/2687
https://chikyu.repo.nii.ac.jp/records/2687
0be0f551-126d-4c51-80be-0995fa8ecafb
名前 / ファイル ライセンス アクション
Amur_Okhotsk_Project_4_11.pdf Dynamic changes of soil organic carbon under different land use type in Sanjiang Plain (6.2 MB)
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Item type 図書の一部 / Book(1)
公開日 2018-11-20
タイトル
タイトル Dynamic changes of soil organic carbon under different land use type in Sanjiang Plain
タイトル
タイトル Dynamic changes of soil organic carbon under different land use type in Sanjiang Plain
言語 en
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_2f33
資源タイプ book
著者 CHI, G.

× CHI, G.

WEKO 2752

CHI, G.

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WANG, J.

× WANG, J.

WEKO 2753

WANG, J.

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LU, C.

× LU, C.

WEKO 2754

LU, C.

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CHEN, X.

× CHEN, X.

WEKO 2683

CHEN, X.

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SHI, Y.

× SHI, Y.

WEKO 2685

SHI, Y.

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ZHOU, L.

× ZHOU, L.

WEKO 2682

ZHOU, L.

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CHI, G.

× CHI, G.

WEKO 2755

en CHI, G.

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WANG, J.

× WANG, J.

WEKO 2756

en WANG, J.

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LU, C.

× LU, C.

WEKO 2757

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CHEN, X.

× CHEN, X.

WEKO 2687

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SHI, Y.

× SHI, Y.

WEKO 2689

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ZHOU, L.

× ZHOU, L.

WEKO 2686

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抄録
内容記述タイプ Abstract
内容記述 The Sanjiang Plain in the northeast part of Heilongjiang Province is one of the largest freshwater marshes in China, which has been experienced intensive cultivation over past 50years. To understand the dynamic changes of soil organic carbon (SOC) after different durations of cultivation, soil samples down to a depth of 120 cm were collected in layers from the lowland and upland fields having been reclaimed for 5-25 years, with adjacent undisturbed wetland and forestland as the control. The study of the vertical distribution of SOC and its relationship with soil pH showed that the SOC content in undisturbed wetland and cultivated lowland rice fields had a marked decrease企om0-10 cm to 40-60 cm and a less change downward, and a similar variation trend was observed in undisturbed forestland and cultivated soybean fields, only with the difference that the SOC content in 0-10cm layer was much higher in forestland than in wetland, and lower in soybean fields than in rice fields. For undisturbed wetland, its SOC content in surface layer was decreased by 49.3% and 14.3% after claimed for 10 and 25 years, and for undisturbed forestland, 81.9% and 68.3% of its SOC in surface layer were lost after reclaimed for 5 years and 18 years, respectively. The soil pH in surface layer was decreased in the sequences of undisturbed wetland > lowland rice field reclaimed for 25 years > lowland rice field reclaimed for 10 years, and soybean field reclaimed for 5 years > soybean field reclaimed for 18 years > undisturbed forestland. All of these suggested that reclamation made a great loss of SOC in surface layer both in wetland and forestland, and the SOC loss was much greater in forestland than in wetland. The variation of surface soil pH under reclamation could be one of the factors inducing the SOC loss, and a longer period of reclamation combining with rational management could be favorable to the stabilization of SOC.
図書名
収録物名 Report on Amur-Okhotsk Project No.4
出版者
出版者 Amur-Okhotsk Project
開始ページ
開始ページ 95
終了ページ
終了ページ 100
出版年月日
日付 2007-02
日付タイプ Issued
ISBN
関連タイプ isPartOf
識別子タイプ ISBN
関連識別子 4-902325-23-2
関連サイト
識別子タイプ URI
関連識別子 http://www.chikyu.ac.jp/AMORE/
関連名称 アムール・オホーツクプロジェクト
関連サイト
識別子タイプ URI
関連識別子 http://www.chikyu.ac.jp/
関連名称 総合地球環境学研究所
フォーマット
内容記述タイプ Other
内容記述 application/pdf
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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