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研究生:王禎祺
研究生(外文):Wang Jen-Chi
論文名稱:台灣酸性土壤石灰需要量之評估
論文名稱(外文):Evaluation of Lime Requirement in Taiwan Acid Soils.
指導教授:何聖賓
指導教授(外文):Sheng-Bin Ho
學位類別:碩士
校院名稱:國立臺灣大學
系所名稱:農業化學研究所
學門:農業科學學門
學類:農業化學類
論文種類:學術論文
論文出版年:1999
畢業學年度:87
語文別:中文
論文頁數:90
中文關鍵詞:石灰需要量
外文關鍵詞:Lime Requirement
相關次數:
  • 被引用被引用:10
  • 點閱點閱:1914
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酸性土壤不適合大多數作物的栽培與生長,施用石灰到酸性土壤中可以將酸鹼度提升到適當的範圍,使土壤中植物營養元素呈現良好的平衡關係,但施用過多的石灰亦會造成營養元素的缺乏或毒害,如何準確評估適當的石灰需要量便是管理酸性土壤最大的課題。
本篇研究採用台灣二十五種酸性土壤,包括表土與底土,以三種不同水份境況的土壤-石灰孵育方法求其石灰需要量,三種水份境況分別是田間容水量、浸水、乾濕交替,並與土壤-鹼滴定法作比較,此外亦採用四種土壤-緩衝溶液平衡法(SMP單一緩衝溶液法、Adams-Evans單一緩衝溶液法、改良式Woodruff單一緩衝溶液法、BaCl2-TEA滴定法(交換性酸度法)),對供試土壤進行測定,以期對台灣酸性土壤石灰需要量速測方法作一評估。
研究結果顯示三種不同水分境況孵育的石灰需要量為田間容水量﹥乾濕交替﹥浸水,且三者之間有良好的相關性。由此可知浸水狀況下,石灰與土壤之間有較完全的反應。土壤-鹼滴定法的結果與田間容水量的結果較為接近,且與三種孵育的結果都有良好的相關性。在高石灰需要量時,四種土壤-緩衝溶液平衡法的結果皆明顯低估。以台灣土壤測定的pH值對鹽基飽和度關係式(pH = 0.0316 × BSP + 3.6485, r2=0.76***)來計算Adams-Evans石灰需要量,可以得到更好的適用性。在此研究中,所有方法得到之石灰需要量都有良好的相關性。
將孵育方法得到之石灰需要量與土壤基本性質作迴歸及相關分析後,可得知所有方法都不只與單一種的土壤性質有良好的相關性,諸如土壤pH值、陽離子交換容量、游離氧化鋁、交換性酸度、有機碳含量,所得到的經驗式(如:田間容水量孵育之LR = 3.07 ×O.C. + 2.27 ×Exchangeable acid + 0.72 ×CEC — 5.40 ×pH + 0.79 ×DCB-Al + 17.15 ,r2=0.95***)可以作為研究台灣酸性土壤石灰需要量的良好指標。
Strongly acidic soils greatly restrict the growth of most plants. The addition of lime raises the soil pH, eliminates the major problems of acid soils, and thus improves plant growth. However, adding excess lime causes soil nutrients imbalance is not desirable and is additional cost. The objectives of this study were to determine lime requirements of twenty five acid soils from Taiwan using various methods, including titration method, CaCO3 incubation method under three moisture conditions, and four buffer method, i.e., SMP method, Adams-Evans method, improved Woodruff method, and exchangeable acidity method; and to evaluate the most suitable methods used in Taiwan agricultural soils. Buffer-indicated lime requirements were relate to CaCO3 incubation-measured lime requirements through regression analysis.
Lime requirements measured by incubation method under three moisture conditions decreased slightly in the order of field capacity incubation, alternately wetting and drying incubation and flooding incubation, and correlated well among each other. Lime requirements determined by the titration method were close to those by incubation method under field capacity and correlated well to those of all the three incubation methods. All of the four buffer methods underestimated lime requirements in high lime-required soils as compared to those by the incubation methods. The use of the relationship between soil pH and base saturation percentage from Taiwan agricultural soils ( pH = 0.0316×) to correct lime requirements by Adams-Evans method had shown to be better applicability to Taiwan agricultural soils. Lime requirements determined by all the methods used in this study were correlated well among each other.
The relationship between lime requirements and soil properties using stepwise procedure proposed the following empirical model: LR = 3.07 ×OM + 2.27 ×Exchangeable acid + 0.72 ×CEC — 5.40 ×pH + 0.79 ×DCB-Al + 17.15 , r2=0.95***, where LR is lime requirement in Mg CaCO3/ha, OC is organic carbon in g/kg, EA is exchangeable acidity in cmol(+)/kg, CEC is cation exchange capacity in cmol(+)/kg, DCB-Al is DCB extractable Al in g/kg. This empirical model can be use to predict lime requirement in Taiwan agricultural soils.
中文摘要 ……………………………………………………………Ⅰ
英文摘要 ……………………………………………………………Ⅲ
目錄 …………………………………………………………………Ⅴ
圖次 …………………………………………………………………Ⅵ
表次 …………………………………………………………………Ⅷ
第一章、 前言 ………………………………………………… 1
第二章、 材料與方法 ………………………………………… 10
第一節 供試土壤 …………………………………………… 10
第二節 供試土壤之理化性質分析 ………………………… 16
第三節 酸性土壤石灰需要量之測定 ……………………… 20
第三章、 結果與討論 ………………………………………… 31
第一節 土壤-石灰孵育的結果 ………………………… 31
第二節 土壤-緩衝溶液平衡法之比較 ……………… 48
第三節 土壤基本性質與石灰需要量之關係 …………… 66
第四章、 結論 ………………………………………………… 77
參考文獻 ………………………………………………………… 78
附錄 …………………………………………………………………82
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