土壤有机矿质复合体研究 Ⅶ.土壤结合态腐殖质的形成特点及其结合特征
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STUDIES ON ORGANO-MINERAL COMPLEXES IN SOIL VII.FORMATION AND BINDING CHARACTERISTICS OF SOIL COMBINED HUMUS
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    摘要:

    本文系统剖析了熊毅-傅积平改进法区分的土壤结合态腐殖质的形成特点,胡、富组成及其结合特征。结果表明:(1)用0.1mol/LNaOH及0.1mol/LNaOH+0.1mol/LNa4P2O7混合液连续浸提的松结态(H1)和稳结态(H2)腐殖质所占的比例随土壤pH升高分别呈减少和增加趋势。统计分析显示H1与游离态铁、铝呈极显着的正相关,与交换性钙呈极显着负相关,H2则与交换性钙呈极显着正相关,而与游离态铁、铝呈极显着负相关,不能被浸提的紧结态腐殖质(H3)与pH及各种胶结物质均无显着关系。(2)松结态腐殖质(H1)的胡富比低于稳结态腐殖质(H2)的胡富比。前者与游离态铝呈显着正相关,后者则与土壤pH和交换性钙呈显着正相关。(3)根据溶出物的元素组成,明确松结态主要是铝、铁键结合的腐殖质,但也包含少部分钙键结合的腐殖质,稳结态则主要是钙键结合的腐殖质。

    Abstract:

    HA and FA composition and binding characteristics of soil combined humus differentiated by the modified Hseung's method were studied. The results obtained are summarized as follows: 1.It was observed that with the rise of soil pH, there was a tendency to increase the loosely combined humus(H1) extracted with 0.1mol/L NaOH from soil and to decrease the stably combined humus(H2) extracted sequentially by a 0.1mol/L NaOH-0.1mol/L Na4P2O7 mixture from the residues. Statistical analysis showed that H1 was very significantly positively correlated to free Fe and Al but negatively to exchangable Ca, and that H2 was significantly positively correlated to exchangable Ca but negatively to free Fe and Al. No significant correlation was found between tightly combined humus(H3) and pH or various binding materials of soil. 2. The ratio of humic acid to fulvic acid (HA/FA) was lower in H1 than in Hz. The former was positively correlated with free A1 and the latter positively with pH and exchangable Ca of soil.3. Elemental analysis results of the extracting solution indicated that H, was actually Al/Fe-combined humus with less Ca-combined humus, and H2 was mainly Ca-combined humus.

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徐建民,袁可能.土壤有机矿质复合体研究 Ⅶ.土壤结合态腐殖质的形成特点及其结合特征[J].土壤学报,1995,32(2):151-158. Xu Jianming, Yuan Keneng. STUDIES ON ORGANO-MINERAL COMPLEXES IN SOIL VII. FORMATION AND BINDING CHARACTERISTICS OF SOIL COMBINED HUMUS[J]. Acta Pedologica Sinica,1995,32(2):151-158.

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  • 在线发布日期: 2013-02-25
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