کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4573047 1629454 2016 7 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Influence of soil pedological properties on termite mound stability
ترجمه فارسی عنوان
تاثیر خواص خاکشناسی خاک بر ثبات تپه موریانه
کلمات کلیدی
فرلزول؛ Vertisol؛ افسردگی Odontotermes؛ هند؛ مصالح؛ شکل تپه موریانه؛ خواص کانی شناسی رس
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• Termite mound density is similar in ferralsol and in vertisol.
• Stability of termite mound aggregates is reduced compared to control.
• Degradation of termite nests by rain is more important in vertisol than ferralsol.
• Termites impact differently soil dynamics depending on the environment.

This study investigated the influence of soil properties on the density and shape of epigeous fungus-growing termite nests in a dry deciduous forest in Karnataka, India. In this environment, Odontotermes obesus produces cathedral shaped mounds. Their density, shape (height and volume) and soil physicochemical properties were analyzed in ferralsol and vertisol environments. No significant difference was observed in O. obesus mound density (n = 2.7 mound ha− 1 on average in the vertisol and ferralsol areas). This study also showed that O. obesus has a limited effect on soil physical properties. No differences in soil particle size, pH, or the C:N ratio and base saturation were measured whereas the C and N contents were reduced and CEC was higher in termite nest soils in both environments. Clay mineralogical composition was also measured, and showed the presence of higher amounts of smectite clays in termite nest soils, which thus explained the increasing CEC despite the reduced C and N content. However, the main difference was the shape of the termite mounds. The degradation of the nests created a hillock of eroded soil at the base of termite mounds in the vertisol while only a thin layer of eroded soil was observed in the ferralsol. The increased degradation of termite mounds in the vertisol is explained by the presence of smectites (2:1 swelling clays), which confer macroscopic swelling and shrinking characteristics to the soil. Soil shrinkage during the dry season leads to the formation of deep cracks in the termite mounds that allow rain to rapidly penetrate inside the mound wall and then breakdown unstable aggregates. In conclusion, it appears that despite a similar abundance, termite mound properties depend to a large extent on the soil properties of their environments.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Geoderma - Volume 262, 15 January 2016, Pages 45–51
نویسندگان
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