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研究生:廖永綜
研究生(外文):Liaw,Yeong-Tzonq
論文名稱:南仁山森林生態系氮之收支與循環之探討
論文名稱(外文):Studies on the Nitrogen Budget and Cycle of Nanjenshan Forest Ecosystem
指導教授:李芳胤李芳胤引用關係
指導教授(外文):Lee,Fang-Yin
學位類別:碩士
校院名稱:國立屏東科技大學
系所名稱:環境工程技術研究所
學門:工程學門
學類:環境工程學類
論文種類:學術論文
論文出版年:1998
畢業學年度:86
語文別:中文
論文頁數:93
中文關鍵詞:氮循環土壤水分掉落物礦化作用
外文關鍵詞:Nitrogen CycleSoil WaterLitterfallMineralization
相關次數:
  • 被引用被引用:5
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本研究之主要目的在探討南仁山森林生態系中氮的收支與循環。在一個森林生態系中,氮的主要來源為大氣的乾、濕沉降與植物殘體的養分回歸,這些養分進入土壤環境後之宿命包括土壤之吸附、植物的吸收、脫氮作用或藉由逕流水與滲流水的攜帶而進入河川與湖泊,形成一個循環。本研究係於南仁山古南仁湖樣區針對此課題進行研究,其項目包括土壤性質與主要養分含量、土壤水之收集與成分分析、掉落物量及其成分、有機質礦化作用、大氣乾、濕沉降量及其成份與湖水水質分析等.本區土壤pH之平均值範圍為4.3∼4.8屬極酸性,有機質含量1.0﹪∼5.34﹪為中、高含量,在土壤質地方面,本試驗區土壤與底泥皆屬細質地之黏土或黏質壤土,至於全氮(0.06∼0.17%)與有效氮之含量,一般而言皆不高,而試驗地土壤中有相當含量之鐵、鋁,分別為7.8∼21.0 g/kg與2.1∼4.6 g/kg。土壤水水樣之酸鹼度介於4.6∼6.2之間,且酸性隨土壤深度之增加而增強,銨態氮(1.31∼2.21 mg/L)的分佈呈現表層高於裡層之現象,湖水(0.50 mg/L)及雨水(0.79 mg/ L)中硝酸態氮含量皆較土壤水(6.70 mg/L)低,且硝酸態氮之含量隨土層深度的增加而有明顯增加的淡,亞硝酸鹽均未被檢出,濃度均在1 mg/L以下。樣區中年掉落物總量為6.56 ton/ha,其中以掉落葉片量最高,平均佔總掉落物量的66.47﹪,各月份間的總掉落物量變異甚大,呈雙峰分佈(3∼5月、7∼9月)。掉落物之平均氮含量為1.04﹪,每年藉由落葉累積於林地的總氮量為68.58 kg/ha,而掉落物中氮含量之季節性變化並不明顯。
由孵育實驗之礦化作用結果可知,孵育前後土壤有機質的月平均增加量為0.18﹪,而無機態氮的平均增加量為123.1 mg/kg,銨態氮為76.3 mg/kg,硝酸態氮為37.7 mg/kg,因無機態氮包含銨態氮、硝酸態氮及亞硝酸態氮,故推估剩餘之9.1 mg/kg為亞硝酸態氮的月平均增加量。由此實驗結果可據以推估,本試驗區有機物之年平均礦化量為銨態氮2783.4 kg/ha*year,硝酸態氮1357.3 kg/ha*year。大氣沉降之分析結果顯示,本地區乾沉降中之四種含氮成分之含量分別為NO2- 0.03 ton/km2、NO3- 0.10 ton/km2、NH4+ 0.012 ton/km2及HNO3 1.53 ton/km2,據此推估四種成份之年沉降量為NO2- 0.3 kg/ha*year 、NO3- 1.0 kg/ha*year
、NH4+ 0.12 kg/ha*year及HNO3 15.3 kg/ha*year,而濕沉降之分析值分別為NO3- 4.13 ton/km2*year,NH4+ 3.87 ton/km2*year,以此結果推估二者之年濕沉降量分別為NO3- 41.3 kg/ha*year,NH4+ 38.7 kg/ha*year,故濕沉降為南仁山地區大氣沉降主要來源。南仁山古湖湖水之pH值範圍4.39∼8.69,硝酸鹽含量為0∼2.7 mg/L ,亞硝酸鹽為0.03 mg/L ,銨態氮為0∼0.4 mg/L。
綜合以上結果發現,此樣區氮之主要來源為大氣沉降中之濕沉降,其供應量約為80.08 kg/ha*year,其次為經由掉落物分解回歸量73.54 kg/ha*year,而以乾沉降量之16.64 kg/ha*year最低。而樣區中氮的輸出量,估計被土壤與底泥吸附者約為103.35 kg/ha*year,經由植物吸收之量為65.58 kg/ha*year,藉由水分攜帶進入湖泊而存在於湖水中之量為1.33 kg/ha*year。由於樣區中土壤屬極酸性且所含之有效性氮並不高,故推斷該生態系因脫氮作用所移出之氮素極微。除此之外,底泥的高氮含量應是底泥中有機質的大量吸附及林地表層土壤顆粒因強力沖蝕而流入湖泊後釋放出所附之氮素之結果。
The objective of this project is to study the nitrogen budget and cycle of Nanjenshan forest ecosystem. At Kuhu experimental area, we explored soil properties, soil water contents, amounts and compositions of litterfall, mineralization of organic matter, dry and wet deposition and lake water quality.
The results of soil property analysis showed that soils to be extremely acidic(pH4.3∼4.8), fine-textured(clay and clay loam), low in organic matter(1.0﹪∼5.34﹪), total(0.06﹪∼0.17﹪)and available nitrogen, but high in "free" Fe and Al. Analyses of soil water samples found their pH values were between 4.6∼6.2, decreasing with increasing depth. The NH4+-N content was higher in surface layers than in bottom layers. Lake water and rain water had higher NO3- content than soil water. Nitrite wa not detectable. The amount of litterfall at the experimental site was 6.56 ton/ha*year. Leaves were the main litterfall component(66.47﹪). There were two pronounced peaks of higher monthly litterfall, occurring during the growing season(from March to May)and during the typhoon period(from July to September). The average nitrogen content of the litterfall was 1.04﹪and the total amounts accumulated by litterfall were 68.58 kg/ha*year.
The results of incubation experiments indicated that the amounts of soil organic matter, inorganic nitrogen, NH4+-N and NO3--N increased about 0.18﹪, 123.1 mg/kg, 76.3 mg/kg and 37.7 mg/kg per month, respectively. Based on these results, the annual inputs of NH4+-N and NO3--N through mineralization were 2783.4 and 1357.3 kg/ha*year, respectively. The annual inputs of NO2-, NO3-, NH4+ and HNO3 from dry deposition were 0.03, 0.10, 0.012 and 1.53 ton/km2, respectively. While NO3- and NH4+ from wet desition were 4.13 and 3.87 ton/km2, respectively. According to this data, the amounts of nitrogen originating from dry and wet deposition were, respectively, 16.64 and 80.08 kg/ha*year. Lake water pH values ranged from 4.39 to 8.69. The respective concentrations of NO3-, NO2- and NH4+ were 0∼2.7, 0.03, and 0∼0.4 mg/L.
Within the studied area, the main sources of nitrogen were dry deposition(16.64 kg/ha*year), wet deposition(80.08 kg/ha*year)and decomposition of litterfall(73.54 kg/ha*year). On the other hand, the nitrogen outputs were soil and sediment absorption(103.35 kg/ha*year), plant uptake(68.58 kg/ha*year), denitrification and release by soil water(1.33 kg/ha*year). Since the soil were extremely acidic and low in available nitrogen, it is assumed that denitrification is negligible.
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