以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討

碩士 === 國立臺北大學 === 土壤環境科學系 === 88 ===   High pH and the presence of CaCO3 usually result in low availability of phosphorus (P) in calcareous soils of Taiwan. Lowing soil pH by acidifying materials to the suitable range is an important practice to reclaim cal careous soils. The researches on the recla...

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Main Author: 趙靖豐
Other Authors: 陳仁炫
Format: Others
Language:zh-TW
Published: 2000
Online Access:http://ndltd.ncl.edu.tw/handle/18970951082297704773
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spelling ndltd-TW-088NTPU30200022016-01-29T04:14:31Z http://ndltd.ncl.edu.tw/handle/18970951082297704773 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討 趙靖豐 碩士 國立臺北大學 土壤環境科學系 88   High pH and the presence of CaCO3 usually result in low availability of phosphorus (P) in calcareous soils of Taiwan. Lowing soil pH by acidifying materials to the suitable range is an important practice to reclaim cal careous soils. The researches on the reclamation of calcareous soils and the behaviors of phosphorus (P) during the reclamation of calcareous soils are limit, and needed to be study and evaluated. The objective of this study was to (1)evaluate the lowing the calcareous soil pH capacities by addition sulfur and aluminum sulfate, and the relationship between the calcareous soil pH buffer capacity and soil preopereties, (2)evaluate the effect of acidifying materials addition on the behaviors of P in calcareous soil. Five different calcareous soil with varying CaCO3 amount were selected in this study. Different amounte of sulfur (S0) and aluminum sulfate [Al2(SO4)3] were added into the soil to adjust soil pH to 4 levels and incubated at 25℃-33 Kpa water content then the amounts added and soil pH were related. The P availability index (solution P, Resin-P and Olsen-P) and the forms of phosphate were also determined. In addition, tow rates of KH2PO3 (0.250 mg kg-1) were added into soil befor and after lowing pH and incubated for same time then the P availability index and the forms of phosphate were detrmined. Results showed that soil pH decreasing with increasing amount of S0 and Al2(SO4)3 applied. The time required to low soil pH to same pH with S0 applicatio longer then that of Al2(SO4)3 applied, but the amount needed was less. General speaking, the contents of solutuon P, Resin-P Olsen-P, Fe, Al-P and Ca-P increased with increasing amount of S0 addition, however, except Fe, Al-P content, the contents of solution P, Resin-P and Olsen-P decreased with addition of Al2(SO4)3. Results also indication the additon sequence of acidifying materials and P did affect the availability of P and the relative changes of P comounds in calcareous soils. In general, higher contents of solution P, Resin-P and Olsen-P found in the treatments of S0 or Al2(SO4)3 addedfirst, followed by P added than that of addition with S0 or Al2(SO4)3 application usually resulted in lower P availability than that of S0 application. 陳仁炫 2000 學位論文 ; thesis 89 zh-TW
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language zh-TW
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sources NDLTD
description 碩士 === 國立臺北大學 === 土壤環境科學系 === 88 ===   High pH and the presence of CaCO3 usually result in low availability of phosphorus (P) in calcareous soils of Taiwan. Lowing soil pH by acidifying materials to the suitable range is an important practice to reclaim cal careous soils. The researches on the reclamation of calcareous soils and the behaviors of phosphorus (P) during the reclamation of calcareous soils are limit, and needed to be study and evaluated. The objective of this study was to (1)evaluate the lowing the calcareous soil pH capacities by addition sulfur and aluminum sulfate, and the relationship between the calcareous soil pH buffer capacity and soil preopereties, (2)evaluate the effect of acidifying materials addition on the behaviors of P in calcareous soil. Five different calcareous soil with varying CaCO3 amount were selected in this study. Different amounte of sulfur (S0) and aluminum sulfate [Al2(SO4)3] were added into the soil to adjust soil pH to 4 levels and incubated at 25℃-33 Kpa water content then the amounts added and soil pH were related. The P availability index (solution P, Resin-P and Olsen-P) and the forms of phosphate were also determined. In addition, tow rates of KH2PO3 (0.250 mg kg-1) were added into soil befor and after lowing pH and incubated for same time then the P availability index and the forms of phosphate were detrmined. Results showed that soil pH decreasing with increasing amount of S0 and Al2(SO4)3 applied. The time required to low soil pH to same pH with S0 applicatio longer then that of Al2(SO4)3 applied, but the amount needed was less. General speaking, the contents of solutuon P, Resin-P Olsen-P, Fe, Al-P and Ca-P increased with increasing amount of S0 addition, however, except Fe, Al-P content, the contents of solution P, Resin-P and Olsen-P decreased with addition of Al2(SO4)3. Results also indication the additon sequence of acidifying materials and P did affect the availability of P and the relative changes of P comounds in calcareous soils. In general, higher contents of solution P, Resin-P and Olsen-P found in the treatments of S0 or Al2(SO4)3 addedfirst, followed by P added than that of addition with S0 or Al2(SO4)3 application usually resulted in lower P availability than that of S0 application.
author2 陳仁炫
author_facet 陳仁炫
趙靖豐
author 趙靖豐
spellingShingle 趙靖豐
以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
author_sort 趙靖豐
title 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
title_short 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
title_full 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
title_fullStr 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
title_full_unstemmed 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
title_sort 以硫磺及硫酸鋁改良石灰質土壤策略下對磷行為的探討
publishDate 2000
url http://ndltd.ncl.edu.tw/handle/18970951082297704773
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