The quality of Muntilan sand (Central Java) as construction material, a longitudinal study

• Main Author: Endroyo, Bambang
• Format: Conference Proceeding
• Language: English
• Subjects: Avalanches; Construction materials; Construction standards; Contractors; Correlation analysis; Domes; Durability; Fineness; Lava; Long term; Longitudinal studies; Organic chemistry; Rivers; Sand; Weight
• ISSN: 0094-243X; 1551-7616
• DOI: 10.1063/1.4945470

Muntilan sand is a volcanic sand generated by the volcanic activities of Mount Merapi which excavated from Muntilan district. Mount Merapi located at Central Java, Indonesia, is still active until now and erupts almost every 5–10 years. It’s eruptions produced the form of lava which later get cold, perched around the peak, and forming lava domes. Furthermore, a part of lava dome avalanches will be slide down through the rivers on the the foot of the mountain. One of several districts which have rivers that containing volcanic materials is Muntilan. Muntilan sand has been used widely as a construction material. The prospects of thiruses were very good and may not be substituted by the other local sand. As a construction material, Muntilan sand must fulfill technical standard (durability number, fineness modulus, unit weight, silt content, organic content, and chemical content). But as a nature material, Muntilan sands also are influenced by circumstance of the environment. The research was conducted to describe the quality of Muntilan sand in a long term (the past until future). The method used was descriptive in longitudinal study and also a meta analysis. The result may useful for contractors and consultants (local, national and international/foreign) which will get a several projects in Central Java. The research conclusions are: (1) Until several years which will come, Muntilan sand was suitable for the construction works,(2) The durability, fineness modulus, unit weight, silt content, and organic content was in a constant rate, and have tend to increase for future, and (3) The chemical content was not in constant rate but varies in long term.