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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 許正一 | zh_TW |
| dc.contributor.advisor | Zeng-Yei Hseu | en |
| dc.contributor.author | 陳維浩 | zh_TW |
| dc.contributor.author | Wei-Hau Chen | en |
| dc.date.accessioned | 2024-07-18T16:10:11Z | - |
| dc.date.available | 2024-07-19 | - |
| dc.date.copyright | 2024-07-18 | - |
| dc.date.issued | 2024 | - |
| dc.date.submitted | 2024-07-12 | - |
| dc.identifier.citation | Adu, J. K., Oades, J. M. 1978. Physical factors influencing decomposition of organic materials in soil aggregates. Soil Biology and Biochemistry. 10, 109-115.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/93134 | - |
| dc.description.abstract | 增加土壤碳匯不僅能提升土壤肥力，亦能減緩溫室效應。農田中不同耕作方式會影響作物產量與土壤中有機碳含量，但僅量測有機碳含量無法判斷土壤中的有機碳是否能穩定保存。因此將有機碳藉由分解的難易度，區分成具有不同物理化學特性的型態，能判斷有機碳在土壤中的周轉速率，了解土壤有機碳品質。然而，目前台灣農田土壤的有機碳型態之相關研究不足。因此，本研究目的為研究台灣北部地區旱田在不同施肥以及水田土壤在不同水分管理下，計算作物生產量與土壤碳匯含量，以及有機碳型態在含量與分布上的變化，以了解台灣農田土壤有機碳的品質。研究區域位於新北市新店區台大實驗農場安康分場，種植狼尾草 (旱田) 以及水稻 (水田)。採集土壤樣品進行有機碳型態分離，分別是低密度態、高密度態、可氧化態及非可氧化態，並分析團粒穩定度、有機碳官能基與微生物之活性。研究結果顯示，在旱田中，化學肥料可提升地上部作物產量，而有機肥料施用則增加了最多的土壤有機碳含量。混合施用有機肥料與硝化抑制劑可維持較佳的團粒穩定度和微生物生長，並提供持續的碳源。在水田不同水分管理下，慣行灌溉具有較高水稻產量，而雨養管理有較高的團粒穩定度和微生物量。在不同水分管理下，土壤有機碳型態分布具有相同趨勢，主要以重密度態儲存。綜合評估地上部產量與土壤有機碳匯及其穩定度，建議旱田採用有機肥料與化學肥料混合施用，水田採用雨養管理，以提升台灣農田土壤有機碳品質。 | zh_TW |
| dc.description.abstract | Increasing soil carbon sequestration not only enhances soil fertility but also mitigates the greenhouse effect. Measuring total organic carbon content cannot accurately reflect the quality of soil carbon sequestration. Therefore, organic carbon is divided into different fractions based on its decomposition difficulty. These fractions exhibit distinct physical and chemical properties in the soil, allowing us to assess the stability of soil organic carbon and understand its quality. However, there is still a lack of research on the organic carbon fractions of farmland soils in Taiwan. Therefore, this study aims to investigate the crop yield and soil carbon sequestration content in uplands under different fertilization practices and in paddy fields under different water management practices in northern Taiwan. The study also aims to analyze the changes in the content and distribution of various organic carbon fractions to understand the quality of soil organic carbon in Taiwanese farmlands. The study area is located in the farmland of the Ankang Branch of NTU Farm, Xindian District, New Taipei City, and is planted with Pennisetum (upland field) and rice (paddy field). Soil samples were collected regularly to separate the fractions of organic carbon, which were the light fraction, heavy fraction, oxidizable fraction, and non-oxidizable fraction. And analyze the aggregate stability, organic matter functional groups, and microbial biomass carbon. The results showed that in the upland, chemical fertilizers increased the yield of aboveground crops, while organic fertilizers increased soil carbon sinks. A mixed application of organic fertilizers with nitrification inhibitors maintains optimal aggregate stability and microbial activity and provides a sustainable source of carbon. Under different water management practices in paddy fields, conventional irrigation had higher rice yields, while rainfed management led to higher aggregate stability and microbial biomass. The distribution of soil organic carbon forms exhibits the same trend under different water management practices, with the majority stored in the heavy fraction. Considering both above-ground yield and the sequestration and stability of soil organic carbon, it is recommended to use a combination of organic and chemical fertilizers in upland fields and adopt rainfed management in paddy fields to enhance the quality of soil organic carbon in Taiwanese farmlands. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2024-07-18T16:10:11Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2024-07-18T16:10:11Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 口試委員會審定書 i
誌謝 ii 中文摘要 iii 英文摘要 iv 目次 ⅵ 圖次 ⅷ 表次 ⅸ 第一章 前言 1 第二章 文獻回顧 3 2.1土壤有機碳特性與有機碳型態劃分 3 2.2判斷土壤有機碳含量與品質的輔助因子 4 2.3農業土地利用及管理對土壤有機質之影響 6 第三章 材料與方法 9 3.1 研究區域、試驗設計及樣品採樣 9 3.1.1旱田試驗設計及樣品採樣 10 3.1.2水田試驗設計及樣品採樣 10 3.2土壤剖面調查與野外型態特徵描述 14 3.3 土壤物化性質分析 14 3.4土壤有機碳型態分離 19 3.5土壤微生物生質碳 21 3.6土壤團粒穩定度 22 3.7固體 13C CP/MAS-NMR 23 3.8 傅立葉轉換紅外光譜FT-IR 23 3.9 AMS碳14定年 24 3.10統計分析 24 第四章 結果與討論 25 4.1土壤物化性質 25 4.2 不同耕作下農田作物產量與土壤有機碳匯28 4.2.1旱田 28 4.2.2水田 30 4.3土壤有機碳型態特性與不同耕作方式後型態分布31 4.3.1旱田土壤 31 4.3.2水田土壤 36 4.4有機碳型態分布與團粒穩定度之關聯 39 4.4.1旱田土壤 39 4.4.2水田土壤 42 4.5有機碳型態分布與微生物生質碳之關聯 44 4.5.1旱田土壤 44 4.5.2水田土壤 46 4.6有機碳型態分布與有機質官能基之關聯 49 4.6.1旱田土壤 49 4.6.2水田土壤 50 第五章 結論 52 第六章 參考文獻 53 第七章 附錄 69 | - |
| dc.language.iso | zh_TW | - |
| dc.subject | 水田 | zh_TW |
| dc.subject | 有機碳型態 | zh_TW |
| dc.subject | 施肥 | zh_TW |
| dc.subject | 土壤碳儲存 | zh_TW |
| dc.subject | 旱田 | zh_TW |
| dc.subject | paddy field | en |
| dc.subject | fertilization | en |
| dc.subject | upland | en |
| dc.subject | soil carbon storage | en |
| dc.subject | organic carbon fractionation | en |
| dc.title | 台灣北部不同耕作方式對土壤有機碳型態分布的影響 | zh_TW |
| dc.title | Fractionation of soil organic carbon affected by different croppings in northern Taiwan | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 112-2 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 王尚禮;鄭智馨 | zh_TW |
| dc.contributor.oralexamcommittee | Shan-Li Wang;Chih-Hsin Cheng | en |
| dc.subject.keyword | 有機碳型態,土壤碳儲存,旱田,水田,施肥, | zh_TW |
| dc.subject.keyword | organic carbon fractionation,soil carbon storage,upland,paddy field,fertilization, | en |
| dc.relation.page | 72 | - |
| dc.identifier.doi | 10.6342/NTU202401495 | - |
| dc.rights.note | 同意授權(限校園內公開) | - |
| dc.date.accepted | 2024-07-12 | - |
| dc.contributor.author-college | 生物資源暨農學院 | - |
| dc.contributor.author-dept | 農業化學系 | - |
| dc.date.embargo-lift | 2029-07-12 | - |
| 顯示於系所單位： | 農業化學系 | |
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