木本植物侵入者Dillenia suffruticosa (Griff.)的影响土壤和地上、地下植物群的理化性质

B. A. K. Wickramathilake, T. Weerasinghe, S. Ranwala
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引用次数: 3

摘要

dillenia suffruticosa (Griffith) Martelli是斯里兰卡湿区低洼地区快速传播的外来入侵物种,目前被列为值得重视的国家重要外来入侵物种。因此,研究了这种木质入侵植物对土壤理化性质和地上、地下植物区系的影响。从Avissawella到Ratnapura的46公里范围内确定了5个采样点。在每个场地,两个相邻的地块[1m x10m]分别用于D。勾勒出存在(D +)和不存在(D -)的suffruticosa。采用标准方法测定土壤理化参数、微生物生物量和菌落数,并采用SPSS统计软件进行D +和D -方差分析比较。在35%和50%水分条件下,采用凋落物袋技术测定了苦参叶的分解速率。采用Jaccard和Sorenson多样性指数对样林地上植物物种丰富度进行了比较。赤芍叶片的分解速度较慢,但与土壤含水量无关,其分解速率大致相同。D +土壤的粒度分布中,大颗粒所占的比例要高得多。D +位点孔隙率较高,表明土壤被曝气。D +的pH值明显低于D -,形成了酸性土壤,而导电性显著提高,使土壤进一步受到胁迫。阳离子交换容量(CEC)的显著下降与土壤肥力有关,是一个值得关注的显著发现。据报道,D +土壤中磷酸盐含量显著增加,这支持了植物入侵者能够增加土壤中磷酸盐含量的观点。D +位点记录的较高生物量值和较高的细菌菌落数量可能与意外记录的较高有机碳有关。Jaccard指数和Sorenson指数均表明,D +和D -位点在地上植物物种丰富度方面存在差异。因此,我们已经确定了地表植被和土壤性质的变化,需要进一步的研究来确定土壤退化的程度。
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Impacts of Woody Invader Dillenia suffruticosa (Griff.) Martelli on Physio-chemical Properties of Soil and, Below and Above Ground Flora
D illenia suffruticosa (Griffith) Martelli, that spreads fast in low-lying areas in wet zone of Sri Lanka is currently listed as a nationally important Invasive Alien Species that deserves attention in ecological studies. Thus, impact of this woody invader on physical, chemical properties of soil and below and above ground flora was investigated. Five sampling sites were identified along a distance of 46km from Avissawella to Ratnapura. At each site, two adjacent plots [1m x10m each for D . suffruticosa present (D +) and absent (D - )] were outlined. Physical and chemical soil parameters, microbial biomass and number of bacterial colonies in soil were determined using standard procedures and compared between D + and D - by ANOVA using SPSS. Rate of decomposition of D. suffruticosa leaves was also determined using the litter bag technique at 35% and 50% moisture levels. Above ground plant species richness in sample stands was compared using Jaccard and Sorenson diversity indices.  Decomposition of D. suffruticosa leaves was slow, but occurred at a more or less similar rate irrespective of moisture content of soil. Particle size distribution in D + soil showed a much higher percentage of large soil particles.  Higher % porosity in D + sites was a clear indication that the soil was aerated.  The pH was significantly lower for D + than D - thus developing acidic soils whereas conductivity has been significantly high making soil further stressed. The significant drop in Cation Exchange Capacity (CEC) in D + soil was a remarkable finding to be concerned with as it correlated with fertility of soil. Significantly higher values of phosphates reported in D + soil support the idea that plant invaders are capable to increase phosphates in soil. Higher biomass values recorded for D + sites together with higher number of bacterial colonies could be related to the unexpectedly recorded higher Organic Carbon. Both  the  Jaccard  and  Sorenson   indices indicated  that  D + and  D - sites  were dissimilar with respect to  above ground  plant  species  richness.  Thus, changes in above ground vegetation and soil properties due to the invasion were identified and further studies are needed for determining the degree of soil deterioration due to the invasive behavior of D. suffruticosa .
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