KARATERISTIK MORFOLOGI TANAH DARI BERBAGAI BAHAN INDUK DI DESA WAKOILA KECAMATAN SAWERIGADI, KABUPATEN MUNA BARAT

Netti Ridha, M. Hemon, Namriah Namriah, Z. Zulfikar, La Ode Rustam, Syamsu Alam
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Abstract

Characteristics of the soil formed are influenced by the parent rock as the original material. Different parent rocks have different physical, chemical, and mineral compositions that affect the different characteristics of the soil formed. This study aims to determine the soil morphology characteristics of various parent materials in Wakoila Village, Sawerigadi District, West Muna Regency. This research was conducted by survey method and field analysis of three parent materials. In the three parent materials, the external characteristics and internal characteristics of the profile were observed. Based on the results of the study showed that the morphological characteristics of the soil from the parent material of gravel (PI), alluvium deposits (PII) and limestone (PIII) have various soil morphological characteristics, both soil color, soil solum depth, horizon thickness, horizon symbol, soil texture, soil structure, soil consistency and soil pores. Soils made from gravel are characterized by a coarser soil texture, whereas soils from limestone tend to have a higher clay content. Meanwhile, soils made from alluvium deposits are characterized by darker soil colors and tend to have more pores.
形成的土壤的特性受母质岩石作为原始物质的影响。不同的母岩具有不同的物理、化学和矿物组成,从而影响形成的土壤的不同特征。本研究旨在确定西穆纳县Sawerigadi区Wakoila村不同母质土壤的形态特征。本研究采用调查法和实地分析三种母材。在三种母材中,观察了型材的外部特性和内部特性。研究结果表明,砾石(PI)、冲积层(PII)和石灰岩(PIII)母质土壤的形态特征具有不同的土壤形态特征,包括土壤颜色、土壤土壤深度、层厚、层符号、土壤质地、土壤结构、土壤稠度和土壤孔隙。砾石制成的土壤具有较粗糙的土壤质地,而石灰石制成的土壤往往具有较高的粘土含量。与此同时,冲积层形成的土壤的特征是土壤颜色较深,气孔较多。
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