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鄂尔多斯高原灌草群落土壤理化性质变化
Authors
姜联合
张瑞红
+4 more
来利明
王永吉
蔡文涛
郑元润
Publication date
1 January 2018
Publisher
Abstract
土壤理化性质的变化对植物群落的演替起着决定作用,探讨灌丛化过程中不同阶段土壤理化性质的变化规律,可为草地生态系统的恢复提供理论依据。以鄂尔多斯高原天然分布的本氏针茅(Stipa bungeana)与油蒿(Artemisia ordosica)过渡区的不同植物群落为研究对象,通过野外调查,选择本氏针茅向油蒿群落过渡过程中不同演替阶段的代表性植物群落,采用环刀法采集土壤样品,分析6个不同群落0-50cm土层土壤理化性质的变化规律。结果表明,在本氏针茅向油蒿群落过渡的过程中,1)0-50cm土层土壤质地发生显著变化(P<0.05),由砂质壤土变为砂土,土壤砂粒含量由阶段Ⅰ的77.5%上升到阶段Ⅵ的89.2%,土壤黏粒、粉粒含量分别由阶段Ⅰ的0.59%和21.9%下降到阶段Ⅵ的0.21%和10.6%;表层土壤含水量由阶段Ⅰ的6%下降到阶段Ⅵ的4%,土壤容重由阶段Ⅰ的1.58g·m~(-3)上升到阶段Ⅵ的1.77g·m~(-3);2)土壤全氮、全碳、全磷总体上呈下降趋势,0-5cm表层土壤的全氮、全碳、全磷分别从阶段I的0.08%、0.77%、0.41%下降到阶段Ⅳ的0.03%、0.25%、0.23%,土壤全钾整体上波动较大。3)土壤表层肥力下降,质量降低,水分含量降低,限制了浅根系草本植物的生长,有利于深根系的半灌木植物油蒿的入侵。在鄂尔多斯高原灌丛化草地生态系统恢复中,应注重提高表层土壤质量,促进灌丛化草地的恢复
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of Botany,Chinese Academy Of Sciences
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Last time updated on 09/06/2022