請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/24406
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 王亞男 | |
dc.contributor.author | Pei-Fen Lan | en |
dc.contributor.author | 藍佩芬 | zh_TW |
dc.date.accessioned | 2021-06-08T05:24:50Z | - |
dc.date.copyright | 2005-07-30 | |
dc.date.issued | 2005 | |
dc.date.submitted | 2005-07-23 | |
dc.identifier.citation | 丁昭義(1999)木材化學。國立編譯館。第157-158頁。
王松永、丁昭義(1984)林產學(上冊)。台灣商務印書錧。第516-533頁。 王巧萍、劉美娟(2003)火燒及植被對七星山土壤溫度及化學性質之影響。台灣林業科學18(1):43-54。 王薇(2004)利用土壤有機質中13C值探討勝光地區植群之改變。國立台灣大 學森林學研究所碩士論文。 林良平(1987)土壤微生物學(上)。南山堂出版社發行。171-244頁。 林良平(1993)土壤微生物學。國立編譯館。193-229頁。 林昭遠、陳明義、呂金誠(1986)林火對對東卯山區台灣二葉松林地土壤沖蝕量及養分流失量之影響。中華水土保持學報17(2):42-49。 林朝欽(1992)台灣地區國有林之森林火分析(1963-1991年)。林業試驗所研究報告季刊7(2):169-178。 林朝欽(1993)國有林大甲溪事業區之森林火災及防火線。林業試驗所研究報告季刊8(2):159-167。 林朝欽(2001)從千禧年美國林火季探討-台灣林火管理策略。台灣林業27(1) :13-17。 林國銓(2002)福山闊葉林四樹種綠葉的分解及氮動態變化。台灣林業科學17(1)75-85。 何淑玲(2003)台灣二葉松松針接種不同真菌對其分解之影響。國立中興大學森林學系研究所碩士論文。 洪富文(1988)台灣中部地區不同年齡杉木人工林內土壤有效氮及硝化作用之潛能。中華林學季刊21(4):39-84。 高清(1989)林木生理學實驗法。國立編譯館。162頁。 黃青萸(2000)南仁山森林落葉層兩棲類與無脊椎動物對落葉分解之影響。國立成功大學生物學系碩士論文。 張正平(1997)南仁山低地雨林凋落物之研究。國立台灣大學植物學研究所碩士論文。 張家豪(2001)南仁山低地雨林凋落物分解及有效性養分研究。國立台灣大學植物學系碩士論文。 楊遠波、劉和義、呂勝由(1998)臺 灣 維 管 束 植 物 簡 誌第 二 卷種子 植物門。中華民國行政院農業委員會出版。 劉美娟、王巧萍(2003)林火對土壤生態系之影響。台灣林業30(1)61-65。 劉棠瑞、蘇鴻傑(1978)大甲溪上游台灣二葉松天然林之植群組成及相關環境因子之研究。國立台灣大學農學院實驗林研究報告121:207-239。 Anderson, J. M. and M. J. Swift(1983)Decomposition in tropical forests. in S. L. Sutton, T., C. Whitmore and A. C. Chadwick(eds.)Tropical Rain Forest: Ecology and Management. pp287-310. Blackwell Scientific Publications. UK. Arunachalam, A., H. M. Pandey, R. S. Tripathi and K. Maithani(1996)Fine root decomposition and nutrient mineralization patterns in a subtropical humid forest following tree cutting. Forest Ecology Management. 86: 141-150. Ando, M(1970)Litterfall and decomposition of some evergreen coniferous forests. Japanese J. Ecology. 20:170-181. Bray, J. R. and E. Gorham(1964) Litter production in forests of the world. Adv. Ecology. Res. 2: 101-187. Berg, B(2000)Litter decomposition and organic matter turnover in northern forest soils. Forest Ecology and Management 133:13-22. Berg, B(1986)Nutrient release from litter and humus in coniferous forest soils-a mini review. Scand, J. For. Res. 1: 359-369. Berg, B., K. Hannus, T. Popoff., O.Theander(1982)changes in organic chemical components of needle litter during decomposition :long-term decomposition in a scots pine forest Ⅰ. Can. J. Bot. 60:1310-1319. Berg, B. and H. Staaf(1981)Leaching, accumulation and release of nitrogen in decomposing forest litter. Ecological Bulletins 33: 136-178. Blair, J. M., R. W. P. Armelee., M. H. Beare.(1990)Decay rates, nitrogen fluxes edcomposer communities of single–and mixed-species foliar litter. Ecology 71(5): 1976-1985. Chen, H., M. E. Harmon., and R. P. Griffiths(2001)Decomposition and nitrogen release from decomposing woody roots in coniferous forests of the Pacific Northwest :a chronsequence approach. Can. J. For. Res. 31: 246-260. Chen, H., M. E. Harmon., R. P. Griffiths., W. Hicks(2000)Effects of temperature and moisture on carbon respired from decomposing woody roots. Forest Ecology Manament 138: 51-64. Chen, M. C., M. C. Wang, C. Y. Chiu., P. M. Huang., and H. B. King(2001)Determination of low molecular weight dicarboxylic acids and organic functional groups in rhizosphere and bulk soils of Tsuga and Yushania in a temperate rain foresst. Plant and Soil 231: 37-44. Collins, H. P., L. F. Elliott., R. W. Rickman., D. F. Bezdicek., R. I. Papendick(1990)Decomposition and interactions among wheat residue components. Soil. Sci. Soc. Am. J. 54: 780-785. Couteaux, M. M. and P. Bottner and B. Berg(1995)Litter decomposition climate and litter quality.Tree 10(2): 63-66. Couteaux, M. M., K. B. Mctiernan, B. Berg, D. Szuberla, P. Dardenne and P. Bottner(1998)Chemical composition and carbon mineralisation potential of Scots pine needles at different stages of decomposition Soil. Biol. Biochem 30(5): 583-595. CNS 2721 木材及紙漿中酸不溶性木質素試驗法。 CNS 4713 木材及紙漿中溶劑萃取物試驗法。 Eric, F., S. K. Nobuhiro., K. Shigeo, and N. Yasuhide(1998)Nutrient dynamics and lignocellulose degradation in decomposing Quercus serrata leaf litter. Ecological Research 13: 199-210. Gardner, W. and H. Hartge (1986) Bluk density. In A. Klute (ed.) Methods of Soil Analysis, Part 1:Physical and Mineralogical Methods.2nd edition. Agronomy monograph. 9:493-544. González-Pérez, J. A., F. J. González-Vila., G.. Almnedros and H. Knicker(2004) The effects of fire on soil organic matter- a review. Environ. Inter. 30, 855-870. Gosz, J. R(1981)Nitrogen cycling in coniferous ecosystem .In Clark , F. E. and T. Rosswall. (eds.) Terrestrial Nitrogen Cycles-Processes, Ecosystem Strategies and Management Impacts, Ecological Bulletins 33: 136-178. Gosz, J. R (1984)Biological factors influencing nutrient supply in forest soil .In : Bowen, G. D. and E. K. S. Nambiar . ( eds. ) Nutrition of Plantation Forests p. 119-146. Hagglund, E(1951)Chemistry of Wood. Acaemic Press, New York. P.326. Ishii, H., S. Katagiri, N. Miyake and S. Sudo(1977)Studies on mineral cycling in a deciduous broadleaved forest at Sanbe forest of Shimane University (Ⅲ) Decomposition rate of A0 horizon and some experiment of leaf decomposition by litterbag method. Bulletin of the Agriculture, sbimane University. 11: 55-59. Jonna, P., T. Levula, and H. Fritze(2004)A reciprocal decomposition experiment of Scots pine needles 19 yr after wood ash fertilization. Soil Biology & Biochemistry 36: 731-734. Joslin, J. D., and G.S. Henderson(1987)Organic matter and nutrient associated with fine root turnover in a white oak stand. For. Sci. 33(2): 330-346. Keyser, P., T. K. Kirk., J. G. Zeikus(1978)Ligninolytic enzyme of Phenerochaete chrysosporium :Synthesized in the absence of lignin in response to nitrogen starvation. J. Becteriol. 135: 790-797. Kim, C., T. L. Sharik., and M. F. Jurgensen(1996)Canopy cover effects on mass loss,and nitrogen and phosphorus dynamics from decomposing litter in oak and pine stands in northern lower Michgan .Forest Ecology Management 80: 13-20. Laode, A. and A. Syoko and H. Akio(2004)Decomposition of leaf litter of four tree species in a subtropical evergreen broad-leaved forest,Okinawa Island, Japan. Forest Ecology Management 202: 1-11. Lousier, J. D. and D. Parkinson(1976)Litter decomposition in a cool temperate deciduous forest. Canadian Journal of Botany 56: 2730-2749. Martinez, Y. A. and J. Sarikhan(1990)Litterfall patterns in a tropical deciduous forest in Mexico over a five-year period. J. Tropical. Ecology 6: 433-444. Mckeague, J. A. , and J. H. Day(1966)Dithionite and oxalate extractable Fe and Al as acids in different various classes of soil. Can. J. Soil Sci. 46: 13-22. Meentemeyer,V., E. O. Box and R. Thompson(1982)World patterns and amounts of terrestrial plant litter production. Bioscience 32(2): 125-128. Mehra, O. P., and M. L. Jackson(1960)Iron oxides removed from soils and clays by a dithionitecitrate system buffered with sodium bicarbonate. Clays Clay Miner 7:317-327. Melillo, J. M., J. D. Aber, A. E. L. Linlins, A. Ricca, B. Fry and K. J. Nadelhoffer(1989)Carbon and nitrogen dynamics along the decay continum: plant litter to soil organic matter. Plant and Soil .115: 189-198. Oades, M (1995) Recent Advances in Organomineral Interaction :Implications for Carbon Cycling and Soil. CRC press/Lewis Publishers,Boca Raton. pp.119-134. O,Connel, A. M(1988)Nutrient dynamics in decomposing litter in Karri forest of South-Western Australia. Soil Biology and Biochemistry. 19: 135-142. Odum , E. P ( 1986 ) Basic Ecology. Saunders Co. Page , A. L (1982) Methods of soil analysis :Part 2 Chemical and Microbiological Properties. American Society of Agronomy. Phillips, M. A. and R. B. Croteau (1999) Resin-based defenses in conifers. Trends in Plant Science 4: 184-190. Robert, L. Tate Ⅲ(1987) Soil Organic Mater Biological and Ecological Effects.John Wiley and Sons. Inc. pp. 1-53. Rhoades, C. C., A. J. Meier., and A. J. Rebertus(2004)Soil properties in fire-consumed log burnout openings in a Missouri oak savanna. For. Ecol. Manage. 192, 277-284. Rhoades , J. D(1982)Cation exchange capacity . In Page , A. L. et al.(ed.) Methods of Soil Analysis ,Part 2: Chemical and Microbiological Properties. Agronomy monograph.9:149-157. Sandhu, J., M. Sinha., and R. S. Ambasht(1990)Nitrogen release from decomposing litter of Leucaena leucocephala in the dry tropics. Soil Biol. Biochem 22 (6): 859-863. Schimel, J. P., S. Helter., and I. J. Alexander(1992)Effects of starch additions on N turnover in Sitka spruce forest floor. Plant and Soil 139: 139-143. Soil Survey Staff(1999)Soil taxonomy: a basic system of soil classification for making and interpreting soil surveys. Agricultural Handbook. no. 436. 2nd ed.Washington, DC:US Govt Print Office. 870p. Staaf, H. and B. Berg(1977)Mobillization of plant nutrient in a Scots pine forest mor in Central Sweden. Silva Fennica 11:210-217. Staaf, H. and B. Berg(1982)Accumulation and release of plant nutrients in decomposing Scots pine needle litter.Long-term decomposition in a Scots pine forest Ⅱ. Canadain Journal of Botany 60: 1561-1568. Smith, V. C. and M. A. Bradford (2003)Litter quality impacts on grassland litter decomposition are differently dependent on soil fauna across time. Applied Soil Ecology. 24: 197-203. Swift, M. J., O. W. Heal. and J. M. Anderson (1979)Decomposition in Terrestrial Ecosystems. Blackwell Science, Oxford. TAPPI(1974)Acid insoluble lignin in wood and pulp. Tecchnical association of the pulp and paper industry. Standard method no: T22205-74. Atlanta, GA:TAPPI press. 2p. Tiessen, H. and J. R. Bettany, J. and W. B. Stewart (1981)An improved method for the determination of carbon in soils and soil extracts by dry combustion. Commun. in Soil Science and Plant Analysis12(3):211-218. Thomas , G. W(1982) Exchangeable cation .In Page, A. L. et al .(ed.) Methods of Soil Analysis, Part 2: Chemical and Micro Biological Properties. Agronomy Monograph. 9:149-157. Tsutomu, E. and H. Kawaguchi(2000)Initial nitrogen content and topographic moisture effects on the decomposition of pine needles. Ecological Research 15:425-434. Turner, J(1975)Nutrient cycling in a Douglas-fir ecosystem with respect to age and nutrient stands. Ph.D. Thesis, University of Washington. Ussiri , A.N. Chris and E. Johnson (2003)Characterization of organic matter in a northern hardwood forest soil by 13C NMR spectroscopy and chemical methods. Geoderma 111 124 (2003) 123–149. Waring, R. H., and W. H. Schlesinger(1985)Forest Ecosystem: Concepts and Management. London: Academic Press. 340p. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/24406 | - |
dc.description.abstract | 本研究選擇勝光地區火燒(2002年5月11日)跡地中人工林內兩種主要樹種二葉松(Pinus taiwanensis Hayata)與栓皮櫟(Quercus variabilis Blume),利用枝葉包法研究野外葉片分解及養分的動態變化,同時比較不同埋置樣點及埋置方式。另外,採用實驗室培養方法研究不同溫度、水分及土壤對栓皮櫟及二葉松葉片分解的影響。
結果顯示,樣區中所選取之三個樣點在土壤基本理化性質上有些許的差異。海拔1830公尺之火燒跡地具有較高的pH值及鹽基陽離子,但有機質含量則較低。CPMAS 13C NMR的分析顯示各樣點中土壤之有機碳官能基極爲相似,均以Aromatic-C爲最多,其次爲O-alkyl-C。研究中所選用的栓皮櫟及二葉松葉片基本性質具有明顯的差異,其中栓皮櫟之氮含量要高於二葉松,而二葉松之木質素含量則高於栓皮櫟。CPMAS 13C NMR分析表示出二種葉片之有機碳官能基也非常相近,均以O-alkyl-C爲主,接近於40%。野外枝葉包分解法則顯示出,在不同處理的方法之下栓皮櫟與二葉松一年之分解量達到60-80%,分解半衰期爲2-7個月。相同方式下,栓皮櫟分解速率快於二葉松;埋入土壤後的分解速率則快於置於地表的處理方式;1830公尺處的分解速率則低於1730公尺處。葉片分解過程中,各種養分均隨時間而損失,但損失程度各有不同,在栓皮櫟中爲P>Mg>>K>Na>C>N>Ca,而在二葉松中爲P>Mg>K>Ca>Na>C>N。13C NMR結果顯示,葉片在分解過程中不同的有機碳官能基基本組成不變。 實驗室的分解培養試驗則顯示,溫度、水分及土壤對落葉分解均有重要的影響。溫度從5℃升高到25℃時,栓皮櫟分解增加49 %,二葉松則增加68 %。當水分從25 %增加到40 %時,栓皮櫟分解降低60 %,二松葉降低30 %。栓皮櫟與二葉松在1730公尺處之土壤中的分解速率其顯著快於1830公尺處之土壤。落葉分解是一個受控於多重因素的過程,不同因素對分解過程的影響程度及重要性則有待更進一步的研究。 | zh_TW |
dc.description.abstract | The objective of this study was to investigate the decompositions and nutrient dynamics of oak(Quercus variablilis Blume) and pine (Pinus taiwanensis Hayata) leaves in a burned site using the litterbag method. The effects of site and buried type on leaf decomposition were also conducted. In the laboratory, the impacts of incubation temperature, soil moisture and type of leaf decomposition were simultaneously considered.Results showed that soil basic physicochemical properties differed from the selected three sites. In the high elevation site, pH value and base cation contents were higher than the other sites, but low organic carbon content was observed. Soil organic carbon functional groups in all sites were similar and dominated by aromatic-C and O-alkyl-C from the results of CPMAS 13C NMR. In the leaf decomposition, oak leaf had higher N and low lignin content than those of pine. Both leaves of oak and pine comprised mainly of O-alkyl-C. According to the results in situ, oak and pine leaves decomposed 60-80% after one year and had a half decomposition time of 2 to 7 months. Results also indicated that oak leaf decomposed faster than pine leaf, leaves decomposed quickly buried in the soil and in the low elevation site. Nutrients released from the leaves during the decomposition varied with time and tree species.Laboratory incubation results showed that high temperature and low soil moisture could result in high decomposition rate of oak and pine leaves. | en |
dc.description.provenance | Made available in DSpace on 2021-06-08T05:24:50Z (GMT). No. of bitstreams: 1 ntu-94-R91625037-1.pdf: 1289578 bytes, checksum: 7e7c5af148d91cafb0f973c5e071c4a6 (MD5) Previous issue date: 2005 | en |
dc.description.tableofcontents | 目錄 ----------------------------------------------------Ⅰ
表目錄 --------------------------------------------------Ⅲ 圖目錄 --------------------------------------------------Ⅳ 中文摘要 -------------------------------------------------Ⅴ 英文摘要 -------------------------------------------------Ⅵ 壹、前言 --------------------------------------------------1 貳、前人研究-----------------------------------------------3 一、火燒的統計---------------------------------------------3 二、落葉的分解---------------------------------------------3 三、落葉的養分變化-----------------------------------------5 四、落葉主要組成成份的變化---------------------------------6 五、影響落葉分解的因素-------------------------------------9 參、材料及方法--------------------------------------------12 一、研究區域概況------------------------------------------12 二、試驗方法----------------------------------------------17 (一)野外試驗--------------------------------------------17 1.土樣分析------------------------------------------------17 2.植體分析------------------------------------------------20 (二)實驗室植體分解--------------------------------------23 肆、結果與討論--------------------------------------------25 一、野外試驗----------------------------------------------25 (一)土樣分析--------------------------------------------25 (二)植體分析--------------------------------------------29 二、實驗室植體分解試驗------------------------------------41 三、討論--------------------------------------------------45 伍、結論--------------------------------------------------48 陸、參考文獻----------------------------------------------50 | |
dc.language.iso | zh-TW | |
dc.title | 火燒跡地二葉松與栓皮櫟葉片之分解 | zh_TW |
dc.title | Foliage Decomposition of Pinus taiwanensis and Quercus variabilis at Post-fire region | en |
dc.type | Thesis | |
dc.date.schoolyear | 93-2 | |
dc.description.degree | 碩士 | |
dc.contributor.coadvisor | 王明光 | |
dc.contributor.oralexamcommittee | 林世宗,邱志郁,蕭英倫 | |
dc.subject.keyword | 火燒跡地,二葉松,栓皮櫟,分解, | zh_TW |
dc.subject.keyword | Post-fire region,Pinus taiwanensis,Quercus variabilis,Decomposition, | en |
dc.relation.page | 57 | |
dc.rights.note | 未授權 | |
dc.date.accepted | 2005-07-23 | |
dc.contributor.author-college | 生物資源暨農學院 | zh_TW |
dc.contributor.author-dept | 森林學研究所 | zh_TW |
顯示於系所單位: | 森林環境暨資源學系 |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-94-1.pdf 目前未授權公開取用 | 1.26 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。