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  • 學位論文

塔塔加地區土壤中氮的礦化和硝化作用

Soil nitrogen mineralization and nitrification in the Ta-Ta-Chia district

指導教授 : 郭幸榮
共同指導教授 : 王明光(Ming-Kuang Wang)

摘要


本研究目的是在探討塔塔加高海拔森林生態系試驗地中,A層 ( 10-20 cm ) 土壤中無機態的銨態氮與硝酸態氮濃度變化,並且估測土壤中無機態氮素的淨礦化速率和淨硝化速率,以及一些環境因子對無機態氮生成的影響。研究時間從2002年的3月至2003年的3月,共採集12次,每次採樣皆三重覆。試驗地分為高山草原 ( 玉山箭竹及紅毛杜鵑灌叢 ) 、台灣鐵杉林區及台灣雲杉林區三個試驗地,並利用野外埋藏袋孵育方法測定土壤中淨礦化及淨硝化速率。結果顯示,土壤中的銨態氮含量,在高山草原區介於 0.79 ~ 12.23 mg N kg -1 之間,台灣鐵杉林區介於 0.96 ~ 16.99 mg N kg-1 之間,雲杉林區則介於 0.71 ~ 9.02 mg N kg-1 之間 ; 土壤硝酸態氮濃度方面,高山草原區介於 0.1 ~ 12.07 mg N kg-1 之間,台灣鐵杉林區介於 1.43 ~ 14.92 mg N kg-1 之間,雲杉林區則介於 8.34 ~ 35.65 mg N kg-1 之間,其中硝酸態氮濃度以雲杉林區的較高。 另外高山草原區的土壤淨礦化速率介於 -0.20 ~ 0.25 mg N kg-1 d-1之間,台灣鐵杉林區介於 -0.32 ~ 0.48 mg N kg-1 d-1之間,雲杉林區則介於 0.23 ~ 5.03 mg N kg-1 d-1之間 ; 高山草原區的土壤淨硝化速率介於 -0.26 ~ 0.23 mg N kg-1 d-1之間,台灣鐵杉林區介於 -0.37 ~ 0.53 mg N kg-1 d-1之間,雲杉林區則介於 0.31 ~ 4.86 mg N kg-1 d-1之間,三個試驗區中以雲杉林區的淨礦化及淨硝化速率為最快,最可能的影響因子包括土壤碎石含量 ( > 2 mm ) 與微生物活性。雲杉林區的總礦化速率對總氮濃度的比例也是三個試驗區中最高。

並列摘要


The objectives of this study were to measure the variation of inorganic nitrogen ( ammonium and nitrate ) concentrations in the soil A horizon ( 10-20 cm depth ), and to determine the net nitrogen mineralization and nitrification rates at Ta-Ta-Chia site of high elevation forest ecosystem. The period of study was from March, 2002 to March, 2003, there were twelve times of sample collections in triplicated of each sampling. The influences of climate and rainfall also were under consideration. The three study sites were covered with different vegetations, including grassland ( Yushania niitakayamensis and Rhododendron rubropilosum Scrub type ), hemlock ( Tsuga chinensis var. formosana ), and spruce ( Picea morrisonicola ) stands. An in-situ buried bag approach was employed to estimate the rates of net N mineralization and nitrification. The soil ammonium concentrations ranged from 0.79 to 12.23 mg N kg-1 soil in grassland, 0.96 to 16.99 mg N kg-1 soil in hemlock, and 0.71 to 9.02 mg N kg-1 soil in spruce stands. Soil nitrate concentrations of grassland, hemlock and spruce ranged from 0.1 to 12.07, 1.43 to 14.92 and 8.34 to 35.65 mg N kg-1 soil, respectively. There were shown a trend of higher soil nitrate concentrations in spruce stand. On the other hand, the net mineralization rate ranged from -0.20 and 0.25 mg N kg-1 d-1 in grassland, -0.32 to 0.48 mg N kg-1 d-1 in hemlock, and 0.23 to 5.03 mg N kg-1 d-1in spruce stand. The net nitrification rates in grassland, hemlock and spruce ranged from -0.26 to 0.23, -0.37 to 0.53 and 0.31 to 4.86 mg N kg-1 d-1 , respectively. Rates of net N mineralization and nitrification, and the ratio of total net N mineralization amount to total nitrogen content in spruce site were higher than those in grassland and hemlock sites. The possible factors influenced these N variations included soil N content, amounts of pebbles ( > 2 mm ) and microbial activity.

參考文獻


洪富文、黃仁欽。1999。土壤樣本處理對於褔山闊葉林土壤現地有效氮估算的影響。台灣林業科學。14(3): 331-337。
江博能。1998。塔塔加鞍部森林、草原土壤間的消長。國立臺灣大學農業化學研究所碩士論文。p. 32-52。
郭魁士。1978。土壤學。p. 299-323。
APHA. 1998. Cadmium reduction method. In M. A. H. Franson (eds.), Standard methods for the examination of water and wastewater. Washington, DC. U.S.A. p. 4-117-118.
Binkley, D., and S. C. Hart. 1989. The components of nitrogen availability assessments in forest soils. Adv. Soil Sci. 10: 57-112.

被引用紀錄


吳俊賢(2007)。塔塔加長期生態研究地區 四種植生土壤之氮礦化及硝化作用〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2007.01925
翁菁羚(2006)。土壤有機氮形態對臺灣中部三種針葉林土壤氮礦化作用之影響〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2006.02243

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