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HANDOUT 1 GEOGRAFI TANAH

HANDOUT 1 GEOGRAFI TANAH. PROGRAM STUDI PENDIDIKAN GEOGRAFI FAKULTAS KEGURUAN DAN ILMU PENDIDIKAN UNIVERSITAS MUHAMMADIYAH SURAKARTA. KLASIFIKASI TANAH. (Horison Diagnostik). Siti Azizah Susilawati, S.Si., MP. Program Pendidikan Geografi, FKIP UMS. EPIPEDON.

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HANDOUT 1 GEOGRAFI TANAH

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  1. HANDOUT 1 GEOGRAFI TANAH PROGRAM STUDI PENDIDIKAN GEOGRAFI FAKULTAS KEGURUAN DAN ILMU PENDIDIKAN UNIVERSITAS MUHAMMADIYAH SURAKARTA

  2. KLASIFIKASI TANAH (Horison Diagnostik) Siti Azizah Susilawati, S.Si., MP. Program Pendidikan Geografi, FKIP UMS

  3. EPIPEDON Horison Epipedon (bhs Yunani, Epi = atas, Pedon = tanah) Ialah horison permukaan (bag.atas) tetapi tidak sinonim dg horizon A (bisa lebih tipis dr A atau bahkan bisa meliputi B).

  4. EPIPEDON 1. Molik (mollis = lunak) : b.o > 1%, wrn lembab (value 3,5), tebal 18 cm, KB > 50%. 2. Antropik (anthropik = manusia) : seperti molik, kandg.phosphat tinggi (P2O5 > 250 pp) sebagai akibat pemupukan yg lama. 3. Histik (histos = jaringan) : b.o tinggi, > 20 % 4. Melanik (melas/melan = hitam) : horiz. Berwrn hitam yg tebal & mgd b.o tinggi berasosiaosi dg mineral amorf (komplek alumunium humus). 5. Umbrik (umbra = bayangan/grey/ndekati hitam) : seperti molik ttp KB < 50 %

  5. 6. Okrik (ochros = pucat) :Horis. wrn terang, b.o < 1 % atau keras-sgt keras dan pejal (masive). 7. Plagen (plaggen = sod/ tanaman sisa2 rumput) : lap.permk.sedalam 50 cm atau lebih dihasilkan dr pemupukan organik yg intensif. EPIPEDON Ialah : horis bwh permukaan

  6. 1.Agrik (ager=lapangan) : horis berada di bawh lapisan olah,terdapat akumulasi humus, debu & lempung. 2. Albik (albus=putih) : horis.bwrn pucat (horiz A2), dlm keadaan lembab value >5. 3. Argilik (argilla=lempung) : horison illuviasi dan akumulasi silikat. 4. Kalsik (calx, calc=kapur): horiz. Illuviasi yg mgd.kalsium karbonat.

  7. 5. Kambik (cambiare=berubah) : suatu horis yg berubah2/ganti2 krn gerakan partikel2 tnh frost, akar & hewan yg luas. 6. Duripan (durus=keras, cadas keras) : horis dibwh permurk. Yg tersementasi oleh illuviasi silikat (Sering mengandung semen tambahan berupa oksida besi dan CaCO3 sehingga warnaberaneka) 7. Fragipan (fragilis=rapuh;cadas yg rapuh):keras bial kering tp rapuh bila lembab, kerapatan partikel tinggi.

  8. 8. Natrik (natrium) : horis. Argilik yg byk mengandung natrium. 9. Oksik (oksida) : akumulasi besi oksida dan Al oksida terhidrat, mineral lempung kaolinit. 10. Petrogypsic (petro=batuan): horis.gypsic yg memadas dan tdk terputus-putus. 11. Placic : padas tipis berwarna hitam sampai merah tua (terikat besi).

  9. Soil Taxonomy Order Suborder Great group Sub group Family Series Soil forming processes / diagnostic horizons Genetic similarity: Wetness, climate, vegetation 12 63 250 1400 8000 19,000

  10. Moisture Conditions Suborder Wet Dry Aquic – poor aeration, reduced iron Udic- dry < 90 total days Ustic - limited but is present Aridic- moist <90 total days Xeric - dry Order Suborder Great group Sub group Family Series Temperature Conditions Family cold Hot Cryic – icy cold Frigid – lower than 8oC Mesic – between 8 and 15oC Thermic – between 15 and 22oC Hyperthermic - > 22oC

  11. 1. Entisols -recent • No diagnostic subsurface horizons. • Very recent or young soil • Little if any profile development • Form on • resistant P.M., • mine spoils, • steep slopes, • floodplains

  12. 2. Inceptisols inception (Latin, beginning) • Slightly more development than Entisols • Young soils but beginning of profile development is evident. • Well-defined profile characteristics of mature soils are yet to be developed. • May have a cambic/umbric horizon

  13. 3. Mollisols mollis (Latin, soft) • Typically form under grasslands. • E.g., Central US • Soils with a mollic epipedon: • Thick humus-rich surface horizon • High % base saturation throughout profile • Slightly leached • Very fertile soils

  14. 4. Alfisolspedalfer • Do have an argillic horizon • About 35% base saturation • Develop in humid, temperate regions • Vegetation is usually deciduous (forests, savanna) • Gray to brown surface horizon • Good for grain production

  15. 5. Spodosols-spodos (Greek, wood ashes) • Have a spodic horizon • Form in humid, cool climates and occur most often in conifer forests (New England, Mich., Canada) • Form in acid, coarse, quartz (sandy) bearing P.M. • Low fertility

  16. 6. Ultisols-ultimate (Latin, last) • Have Argillic or Kandic with <35% Base saturation. • Common in S.E. US, humid tropical, and subtropical regions • Warm and humid environs. • Old, highly weathered, high degree of development (ult) • Low fertility

  17. 7. Oxisols-oxide (French, oxide) • Have an oxic horizon. • Dominated by residual accumulations of Fe and Al oxides and kaolinite • Most extensively weathered soils (occur in tropical regions). • Intense red or yellow (high in oxidized iron). • Low % Base Saturation. • extensively leached • Low fertility.

  18. 8. Histosols-histos (Greek, tissue) • Organic soils (peats and mucks) • Mainly found in cold climates (Alaska, Canada, Finland, Russia) • Low-lying swampy areas • Virtually all Histosols occur in wetland environments • Have very low bulk densities and very high water holding capacity

  19. 9. Vertisols -invert (Latin, turn) • High clay soils (>30% sticky shrink-swell clays). • Deep cracks upon drying • Materials from soil surface fill cracks and become part of the subsurface when the cracks close (inverted soil)

  20. 10. Aridisols-arid (Latin, dry) • Form in aridic moisture regimes (dry) • Dry at least 6 months • Low OM • Little leaching • High base sat. • Can be very productive if irrigated

  21. 11. Andisols-ando (Jap., black soil) • Form from P.M. of volcanic origin • Soil forms by rapid weathering of volcanic ash to produce poorly crystallized aluminosilicates (allophane & imogolite) • Andisols are young soils ( and they have high OM) • In dry climates, can be susceptible to wind erosion • Can have unusually low bulk densities

  22. 12. Gelisols-gelid (Greek, cold) • Presence of permafrost layer within 100 cm of soil surface defines this soil class • Young soils with little profile development • Cold temperatures and frozen conditions for much of the year slow the process of soil formation. • May show evidence of cryoturbation • physical disturbance of soil material caused by freezing and thawing

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