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KLASIFIKASI TANAH

KLASIFIKASI TANAH. AASHTO. AASHTO stands for American Association of State Highway and Transportation Officials.AASHTO proposed soil classification in 1929 and had undergone several revisions till now.

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KLASIFIKASI TANAH

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  1. KLASIFIKASI TANAH AASHTO

  2. AASHTO stands for American Association of State Highway and Transportation Officials.AASHTO proposed soil classification in 1929 and had undergone several revisions till now. It is widely used to classify soil for construction of roads, highways, and airfield (runways, taxiways) especially for subgrade material. Pre-requisites of AASHTO soil classification system are: 1) Mechanical analysis 2) Liquid limit 3) Plasticity Index

  3. Grain Size: 1) Gravel: Fraction passing 75mm sieve and retained on #10 (2mm) US sieve 2) Sand: Fraction passing #10 sieve and retained #200 sieve 3)  Silt and Clay: Fraction passing #200 sieve

  4. Plasticity: 1)                  Term silty is applied when fine fractions have a PI < 10 2)                  Term clayey is applied when fine fractions have PI > 11 Note:   If cobbles and boulders (larger than 75mm) are encountered, they are excluded from the portion of the soil sample on which classification is made. However, %age of such material is recorded.

  5. A1 ~ A3 A4 ~ A7 Granular Materials  35% pass No. 200 sieve Silt-clay Materials  36% pass No. 200 sieve KLASIFIKASI UMUM(AASHTO) • 8 groups: A1~ A7 (dengan sub grup) dan tanah organikA8 • Percobaan yang dibutuhkansieve analysis dan Atterberg limits. • Group index dengan formula, empiris untuk mengevaluasi tanah dalam subgrup • Tujuan pengklasifikasi adalah untuk konstruksi jalan • ( lapisan subgrade) LL and PI untuk memisahakan tanah kelempungan dan kelanauan (hanyaA2 ) LL dand PI untuk memisahkan lanau dan lempung

  6. Group Index For Group A-2-6 and A-2-7 F200: percentase lolos saringan.200

  7. Klasifikasitanahberbutirkasar(kurang35% lolossaringan 200)

  8. Klasifikasitanahberbutirhalus(lebih 35% lolossaringan 200)

  9. Group A-1.     The typical material of this group is a well-graded mixture of stone fragments or gravels, coarse sand, fine sand, and a non-plastic or sligthly plastic soil binder. This group also includes stone fragments, gravels, coarse sand, volcanic cinders etc, without a well-graded binder of fine material. • Subgroup A-1-a includes those materials consisting predominantly of stone fragments or gravel, either with or without a well-graded binder of fine material. • Subgroup A-1-b includes those materials consisting predominantly of coarse sand with or without a well-graded soil binder. • ·         Group A-3.     The typical material of this group is fine beach sand or fine desert blown sand without silty or clayey fines or with a small amount of non-plastic silt. This group includes also stream-deposited mixtures of poorly graded fine sand and limited amounts of coarse sand and gravel.

  10. Group A-2 .     This group includes a wide variety of “granular” materials, which are at the borderline between the materials falling in groups A-1 and A-3 and the silty-clay materials of group A-4 through A-7. It include any materials not more than 35% of which passes a #200 sieve and which cannot be classified as A-1 or A-3 because of having fines content or plasticity, or both, in excess of the limitations for those groups. ·          GroupA-4.     The typical material of this group is a non-plastic or moderately plastic silty soil 75% or more of which usually passes the #200 sieve. The group also includes mixture of fine silty soil and up to 64% of sand and gravel retained on the #200 sieve. ·          Group A-5.The typical material of this group is similar to that described under Group A-4, but it may be highly elastic, as indicated by high liquid limit.

  11. GroupA-6.     The typical material of this group is a plastic clay soil 75% or more of which usually passes the #200 sieve. The group also includes mixtures of fine clayey soil and up to 64% of sand and gravel retained on the #200 sieve. Materials of this group usually have high volume change between wet and dry states. ·           GroupA-7. The typical material of this group is similar to that described under Group A-6, but it has the high liquid limits characteristics of the A-5 group and may be elastic as well as subject to high volume change.

  12. Subgroup A-7-5 includes those materials which have moderate plasticity indexes in relation to liquid limit and which may be highly elastic as well as subject to considerable volume change. ·Subgroup A-7-6 includes those materials which have high plasticity indexes in relation to liquid limit and which are subject to extremely high volume change. ·        Group A-8.     The typical material of this group is peat and muck soil ordinarily found in obviously unstable, swampy areas. Characterized by: ·    low density ·    high compressibility ·    high water content and ·    high organic matter content.

  13. TentukanKlasifikasi Tanah A dan B

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