DAFTAR
PUSTAKA
Adiningsih, S. 1992. Peranan efisiensi penggunaan pupuk untuk melestarikan swasembada
pangan. Orasi pengukuhan Ahli Peneliti Utama.
Puslittanak, Badan Litbang
Pertanian, Dept. Pertanian Bogor, April 1992.
Baak,
J . A. 1949.
Acomprehensive study on recent ashes of the Java volcanoes Semeru,
Kelut
&Merapi. Communication General Agric. Experiment Station, Bogor. No.
8 3 .Besoain, M. E. 1969. Clay mineralogy of volcanic ash soils. In: Volcanic ash soils in
Latin America. Training and Research Center of the IAAIS Tumalba, Costa Rica.
B11-B116
Birrell, K. S. 1965. Some properties of volcanic ash soils. Meeting on the class. and corr.
of soils from volcanic ash. FAO-Report Rome 14:74-8 1
Blakernore, L. C., P. L. Searle, and B. K. Daly. 1981: Soil Bureau Laboratory Methods.
A methods for chemical analysis of soils N.Z. Soil Bureau. Sci Rep., 10A. DSIRO,
New Zealand.
Bouma, J.,
C. A. Fox and R. Miedema. 1990. MicromorphoIogy of hydromorphic soils:
Applications for soil genesis and land evaluation. In: L.A. Douglas (ed.). Soil
Micromorphology:
ABasic and Applied Science. Developments in Soil Science
19.
Elsevier. Amsterdam. p. 257-278.
Brady, N. C. 1981. Soil factors that influence rice production.
In:
Institute of Soil
Science, Academia Sinica (ed.).
Proceedings of Symposium on Paddy Soil.
Science Press, Beijing. Springer-Verlag. Berlin Heidelberg New York. p. 1-19.
Breemen,
N. van, P. Buurman and R. Brinkman. 1992. Processes in Soils. Text for
Course J050-202. Dept. Soil Science and Geology. Agricultural University
Wageningen.
-
Bullock, P.,
N.Feddoroff, A. Jongenius, G. Stoops and T. Tursina. 1985. Handbook for
Soil Thin Section Description. Waine Research Publication, 152p.
Buol, S. W.,
F.D. Hole and R.
J.McCracken.
1980.Soil Genesis and Classification. 2nd
ed. The Iowa State Univeristy Press, Ames.
Buringh. P. 1970.
Volcanic ash soils of the tropics
and
subtropics.
Agr. Univ.
Wageningen. 46pp.
Chadwick,
0.
A , D. M.Hendricks and W. D. Nettleton. 1987a. Silica in duric soils: I.
Adepositional model. Soil Sci. Soc.
A m .J.
51:975-982
Chadwick,
0.
A.,D.
M.Hendricks and
W.D. Nettleton. 1987b. Silica in duric soils:
11.Mineralogy. Soil Sci. S o c
A m .J. 5 1: 982-985
Chadwick,
0.
A.and
W .
D.Nettleton. 1990. Micromophological evidence of adhesive
and cohesive forces in soil
cementation.
In:
L.A. Douglas (ed.).
Soil
~
Micromorphology:
ABasic and Applied Science. Developments in Soil Science
19. Elsevier. Amsterdam p. 207-212.
Chartres, C.
J.and J.
D.Fitzgerald. 1990. Properties of siliceous cements in some
Australian soils and sproftes.
In:
L.
A.Douglas (ed.). Soil Micromorphology: A
Basic and Applied Science. Developments in Soil Science 19. Elsevier.
Amsterdam, p. 199-205.
Chatres, C. J. and L. D. Norton. 1994. Micromorphological and chemical properties of
Australian soils with hardsetting and duric horizons.
In
Ringrose-Voase,
A.J.and
G.S. Humpreys (eds).
Soil Micromorphology: Studies in Management and
Genesis. Elsevier. Amsterdam, p. 825-844.
Childs, C.
W., N.Matsue and
N.Yoshinaga. 1990. Femhydrite in volcanic ash soils in
Japan. Soil Sci. Plant Nutr.. 37(2):299-3 11
Dahlgren, R. 1994. Quantification of allophane and imogolite.
In:
Quantification
Methods in Soil Mineralogy, SSSA Miscellaneous Publication, p. 430-45 1
Dahlgren, R., S. Shoji and M. Nanzyo. 1993. ~ n e r a l o g i c a l
characteristics of volcanic ash
soils.
In:
Shoji, S., M. Nanzyo and R.
Dahlgren (eds.). Volcanic Ash Soils:
Genesis, Properties and Utilization. Elsevier. Amsterdam. p. 101
-
143.
Dames, T. W.
G. 1955. The soils of East Central Java, Contrib. Gen. Agric. Res. Stn.
14 1, Bogor, Indonesia.
Darea. 1989. Perkembangan dan produktivitas tanah
dari lahan sawah clan ladang erupsi
G. Merapi di DL Yogyakarta.
Tesis Magister Sains. Program Studi
Tanah,
Program Pascasarjana
IPB.Delvigne,
J.and
G.Stoops. 1990. Morphology of
mineral
&eathering and neoformation.
I. Weathering of most common silicates.
In:
L.A. Douglas
(ed.).
Soil
Micrornorphology: A Basic and Applied Science. Developments in Soil Science
19. Elsevier. Amsterdam, p. 471481.
Drees,
L.R., L.
P.Wilding, N.
E.Smeck and
A. L.Senkayi. 1989. Silica in soils: Quartz
and disordered silica polymorphs. If7
:Dixon,
J . B .and S.B. Weed (eds.). Minerals
in Soil Environments. SSSA. Madison, Wisconsin, USA. p. 913-974.
Driessen, P.
Mand F.
R.Moormann. 1985. Soils on which rice-based cropping systems
are practiced. In: Soil Physics and Rice. IRRI, Los Banos, Laguna, Philippines.
p. 45-56.
Dudas, M. J. and M. E. Harward. 1975a. Weathering and authigenic halloysite in soil
developed in Mazama Ash. Soil Sci. Soc. Am. Proc. 39: 561-571.
Dudas, M. J. and M. E. Harward. 1975b. Inherited and detrital2
: 1type phyllosilicates in
soils developed in Mazama Ash. Soil Sci. Soc. Am. Proc. 39: 572-577.
Eswaran,
H
1989.Classification of rice
growing soils. In
:Classification and
Management of Rice Growing Soils. Food and Fertilizer Technology Center for
the Asian and Pacific Region. Taiwan. p. 28-32.
Fanning, D. S. and M. C. B. Fanning. 1989.
Soil Morphology;
Genesis, and
Classification. John Wiley
&Sons. New York.
aFlach, K.
W.and
0.
W.Rice, Jr. 1981. Principles of classification
as
applied to paddy
soils. Iir:
Institute of Soil Science, Academia Sinica (ed.). Proceedings of
Symposium on Paddy Soil.
Science Press, Beijing.
Springer-Verlag. Berlin
Heidelberg New York. p. 381-386.
Flach, K. W, T. J. Nimlos and R. J. Engel. 1994. Criteria and classification of indurated
volcanic ash soil horizons.
In. Trans. 15th World Soil Sci. Congress, Acapulco,
Symposium ID 13, The Indurated Volcanic soils. 6a:
481 4 8 6 .
Flach, K.
W., W.D. Nettleton and 0. A. Chadwick. 1992a. Micromorphology
as
a tool
for characterizing silica-indurated materials.
In: ler S i p o s i o Internacional, Suelos
Volcanicos Endurecidos (Uso y Maneja de Tepetates. Colegio de Fostgraduados
Montacillo, Mexico. p. 1-1 7.
Flach, K.
W.,
W.D. Nettleton, and
0. A. Chadwick. 1992b. The criteria of duripans in
the U.S. Soil Taxonomy and the contribution of micromorphology to characterize
silica indurated soils.
In:
Suelos Volcanicos Endurecidos, Terra, Vol. 10, numero
especial, Materiales del I Simposio Internacional, p. 34-45.
Flach, K .
W., W.D Nettleton, L. H. Gile and
J. G. Cady. 1969.
Pedocernentation:
induration by silica, carbonates, and sesquioxides in the Quaternary. Soil Sci.
Flach, K.
W., W. D.Nettleton and R.
E.Nelson. 1974. The micromorphology of silica-
cemented soil horizons in Western North America. In: G.K. Rotherfold (ed.).
Soil Microscopy. 4th International Working-Meeting in Soil ~cromorphology
at
the Dept. of Geography, Queen's University, Kingston, Ontario, Canada, p. 714-
729.
Ghildyal, B. P. 1969. Soil compaction- a new system of rice cultivation. Indian Farming
19: 19-22
Ghildyal, B. P. 1978. Effect of compaction and puddling on soil physical properties and
rice growth.
In:
Soils and Rice. The International Rice Research Institute. Los
Banos, Laguna, Philippines. p. 3 17-336
Gong Zitong. 1983. Pedogenesis of paddy soils and its significance in soil classification.
Soil Sci. 135: 5-10
Gong Zitong. 1986.
Origin, evolution and classification of paddy soils
inChina.
Advanced in Soil Science
5:179-200.
Grant, C. J. 1965. Soil characteristics associated with the wet cultivation of rice.
In.
IRRI.
The Mineral Nutrition of the Rice Plant. Los Banos, Philippines, Johns
Hopkins Press, Baltimore, Maryland. p. 1 5-28.
Hendricks, D. M. and L. D. Whittig. 1968a. Andesite weathering. I. Mineralogical
transformations &om andesit to saprolit.
J. Soil Sci. 19: 135-146.
Hendricks, D. M. and L. D. Whittig. 1968b. Andesite weathering.
II.
Geochemical
changes from andesite to saprolit. J. Soil Sci., 19: 147-153.
Hirokawa.
0. 1980. Introduction to description of volcanoes and volcanic rocks.
Directorate General Jendral Pertambangan Umum.
Pusat Pengembangan
Teknologi Mineral. Bandung Indonesia.
Holmgren, G. G. S. 1967. A rapid citrate-dithionite extractable iron procedure. Soil Sci.
SOC.
Am.Proc. 31: 210-211.
ICOPYLANTH. 1998. Circular Letter No. 3.
January
15,1998. Available
on:http://wwwscas.cit.cornell.edu/icotnanth
I N . 1997. Indonesia.
In: IRRI-CIAT Rice Almanac. 2nd ed. International Rice
Research Institute. The Philippines, p. 82-84
JCPDS. 1974. Selected Powder Diffraction Data for Minerals. Data Book.
l*ed.
Joint
Committee on Powder Diffraction Standards. Pennsylvania. USA.
Jenny,
H.1941. Factors of Soil Formation. McGraw Hill Book Co. Inc. New York.
Kanno, I. 1978. Genesis of rice soils with special reference to profil development. In:
Soils and Rice. The International Rice Research Institute. Los Banos, Laguna,
Philippines. p. 237-254.
Karathanasis, A.
D.1989. Solution chemistry of fiagipans
-
Thermodynamic approach t o
understanding fragipan formation.
In: N. E. Smeck and E.J. Ciolkosz (eds.).
Fragipans: Their Occurrence, Classification and Genesis.
SSSA Special
Publication No. 24. SSSA, Inc. Madison, Wisconsin, USA. p. 113-140.
Kawaguchi, K and K. Kyuma. 1977. Paddy Soils in Tropical Asia. Their material nature
and fertility. Monograph of the Center for Southeast Studies Kyoto University.
The University Press of Hawaii. Honolulu, USA.
Kerr, P. F. 1959. Optical Mineralogy. McCraw-Hill Book Company, Inc. New York.
Koenigs, F. F. F. R. 1950. A 'sawah' profile near Bogor (Java). Contr. of the General
Agric. Research Station, Bogor. No. 15.
Koga,
K.1992. Introduction to Paddy Field Engineering. Asian Institute of Technology.
Bangkok. Thailand.
Kustiawan, 1. 1997. Permasdahan konservasi lahan pertanian dan implikasinya terhadap
penataan ruang wilayah. Studi Kasus: Wilayah Pantura Jawa Barat. Jurnal PWK.
X(1): 49-60
Kyuma, K. 1989. Rice soils of Asia: Distribution and management.
In.
Extension Bull.
No. 292. ASPAC. Food
&Ferttilizer Technology Center: 15-28.
Landon, J. R. 1988. Booker Tropical Soil Manual. Booker Agriculture International
Limited.
Luzio, W, and T. Palma. 1994. Indurated horizons in poorly
drained
volcanic soils from
Chile.
In
:Trans. 15th World Soil Science Congress, Acapulco, Symposium ID 13,
The Indurated Volcanic Soils. 62:
516-527.McKeague,
J. A., J.E. Brydon, and
N. M.Miles. 1971. Differentiation of forms of
extractable iron and alumunium in soils. Soil Sci. Soc. Am. Proc. 3 5: 33-38
McKeague, J. A. and J. H. Day. 1969. Oxalate-extractable
Al
as
criterion for identifying
Mehra,
0. P. and M. L. Jackson. 1960. Iron oxide removal from soils and clays by a
dithionite-citrate system buffered with sodium bicarbonate.
Clay and Clay
Minerals. Vol
5: 31 7-3
27Mitsuchi, M. 1981. Characteristic feature of paddy soils of Japan.
In:Institute of Soil
Science, Academia Sinica (ed.).
Proceedings of Symposium on Paddy Soil.
Science Press, Beijing. Springer-Verlag. Berlin Heidelberg New York.
p.419-
427.
Mitsuchi, M. 1992. Micromorphological observation of wet lowland soils japan.
J. Soil
Sci. Plant Nut.
63:169-176.
Mizota, C , and L. P . Van Reeuwijk. 1989. Clay mineralogy and chemistry of soils formed
in volcanic material in diverse climatic regions.
Soil Monograph
2.ISRIC,
Wageningen, 185 pp.
Mohr, E. C. J. 1944. The Soils of Equatorial Regions with Special Refference to the
Netherlands East Indies. Translated from the Netherlandsch by R.L. Pendleton.
J.W.Edwards. AnnArbor.4
Mohr, E. C. J. and F.
A,van Baren. 1960. Tropical Soils. A critical study of Soil Genesis
as Related to Climate, Rock and Vegetation. Les Editions
A.Manteau S.A.
-
Bruxelles.
Mohr, E. C. J., F.
A.van Baren and,
J. van Schuylenborgh. 1972. Tropical Soils. A
Comprehensive Study of Their Genesis. 3rd revised
a n denlarged ed. Mouton-
Ichtiar Baru-Van Hoeve, The Hague-Paris-Djakarta.48 1p.
Moormann,
F.R. 198 1. The classification of "paddy soils" as related to Soil Taxonomy.
In: Institute of Soil Science, Academia Sinica (ed.). Proceedings of Symposium
on Paddy Soil. Science Press, Beijing. Springer-Verlag. Berlin Heidelberg New
York. p. 139-150.
Moormann, F. R. and
N.van Breernen. 1978. Rice: Soil, Water, Land
IRRI.
Los
Banos, Laguna, Philippines.
Moormann,
F. R. and H. T. J. van de Wetering. 1985. Problems in characterizing and
classifying wetland soils.
In:
Wetland Soils: Characterization, Classification and
Utilization.
IRRI.Los Banos, Laguna, Philippines.
p. 53-
68.
Mulyanto, B. 1995. Characteristic and genesis of minimum distributed soils of two
watersheds in West Java, Indonesia. PhD-Thesis. RUG, Gent.
Munir,
M.1987. Pengaruh penyawahan terhadap morfologi, pedogenesis, elektrokimia
dan klasifikasi tanah. Disertasi Doktor. Program Pascasarjana.
IPB.Nahon,
D. B.1991. Introduction
tothe Petrology of Soil and Chemical Weathering.
Wiley New York. 3 13p.
Nettleton,
W.D., R. B. Daniels and R.
J. McCracken. 1968. Two North Carolina coastal
plain catenas:
I.Morphology and fragipan genesis. Soil Sci. Soc.
Am.Proc. 32:
577-58
1.Nettleton, W. D., R.
J.McCracken and R.
3.
Daniels. 1968. Two North Carolina coastal
plain catenas:
I 1Micromorphology, composition, and fragipan genesis. Soil Sci.
SOC.
Am.Proc. 32: 582-587.
Nimlos, T.
J.1992. Reclamation of indurated volcanic ash materials in Latin America.
Adv. Soil Sci. 17: 153-170
Norton,
L.D. 1994. Micromorphology of silica cementation in soils.
In
Ringrose-
Voase,
AJ. and
G. S. Humpreys (eds).
Soil Micromorphology: Studies in
Management and Genesis. Elsevier. Amsterdam. p. 8 1 1-824
Oleschko,
K, C. Zebrowski, P.Quantin, N. Fedoroff and E. Osores. 1994. Hardened
volcanic soils (Tepetate) in Mexico: Their
geological, pedological or
anthropological origin.
In:
Trans. 15th World Soil Science Congress, Acapulco,
Symposium B. Micromorphological Indicators of Anthropological effects on Soils
6a: 229-249.
Parfin, R. L. 1980. Chemical properties of variable charge soils.
In:
B. K. G. Theng (ed.)
Soil With Variable Charge. N.Z. Soc. Soil Sci., Lower Hutt,
p. 167-194.
Parfitt,
R. L.and A.
D.Wilson. 1985. Estimation of allophane and halloysite in three
sequences of volcanic soils,
New Zealand. In: Caldas, E.F. and D.Y. Yaalon
(eds.). Volcanic Soils: Weathering and Lanscape Relationships of Soils on Tephra
and Basalt. Catena Supplement 7. p. 1-8.
Parfitt, R. L. and J. M. Kimble. 1989. Conditions for formation of dophane in soils. Soil
Sci. SOC.
Am. J.53: 971-977.
Partitt,
R. L., M.Russell and
G. E.Orbell.
1983.Weathering sequence of soils fiom
volcanic ash involving alophane and halloysite. Geoderma 29: 41-59.
Parfitt, R. L., M. Saguisa,
and
J. D. Cowee. 1984. Allophane
and
halloysite formation in
a volcanic ash bed under different moisture condition. Soil Sci. 138: 360-364.
Parfitt, R. L., R. J. Furkert and T. Henmi. 1980. Identification and structure of two types
of allophane from volcanic as soil and tephra. Clay Clay Miner. 28: 328-334
Paterson, E, and R. Swaffield. 1987. Themal Analysis.
117:
Wilson, M.J. (ed). A
Handbook of Determinative Methods in Clay Mineralogy. Blackie. Glasgow and
London. p. 99-132
Patrick, Jr., W. H. 1981. The role of inorganic redox systems in controlling reduction in
paddy soils.
Dr:
Institute of Soil Science, Academia S i ~ c a
(ed.).
Proceedings of
Symposium on Paddy Soil.
Science Press, Beijing.
Springer-Verlag. Berlin
Heidelberg New York. p. 107- 1 17.
Patrick, Jr.,
W.H. and R. D. Delaune. 1972. Characterization of the oxidized and reduced
zones in flooded soil. Soil Sci. Soc.
Am.Proc. 36: 573-576
Pomamperuma, F. N. 1965. Dynamic aspecs of flooded soils.
In:
IRRI. The Mineral
Nutrition of the Rice Plant,
Los Banos, Philippines, Johns Hopkins Press,
Baltimore, Maryland. p. 295-328.
Pornampemma, F.
N.1972. The chemistry of submerged soils. Adv. Agron. 24: 29-96.
Ponnampemma, F.
N.1981. Some aspects of the physical chemistry of paddy soils.
In:
Institute of Soil Science, Academia Sinica
(ed.).
Proceedings of Symposium on
Paddy Soil. Science Press, Beijing. Springer-Verlag.
B e r h Heidelberg New
York. p. 59-94.
Prasetyo, B. H., M. Sukardi dan H. Subagyo. 1996. Tanah-tanah sawah intensifikasi di
Jawa: Susunan mineral, sifat-sifat
kimia
dan Klasifikasinya.
Pemberitaan Pen.
Tanah d m Pupuk 14: 12-24
Quantin, P. 1994. Introduction to knowledge and management of indurated volcanic soil
horizons.
In
:Trans. 15th World Soil Science Congress, Acapulco, Symposium
ID 13, The Indurated volcanic soils. 62: 436444.
Rahardjo,
W., Sukandmmidi dan
H. M. D. Rosidi. 1977.
Peta geologi lembar
Yogyakarta, Jawa.
Skala 1
:100.000.
Direktorat Geologi, Departemen
Pertambangan Republik Indonesia.
Reeuwijk,
L.P.
van.1987. Procedures for soil analysis. 2nd ed. ISRTC.
Reksowirogo,
L.D. 1979.
Merapi.
DaZam: Data Dasar Gunungapi Indonesia.
Direktorat Vubnologi, D i e n Pertambangan Umum, Dep. Pertambangan
dan
Energi, Rep. Indonesia. Hal. 250-280.
Sanchez,
P.A.
1973.Puddling tropical soils. Soil Sci.
115: 149-158, 303-308Schwertmann, U.
1993.Relation between iron oxides, soil color and soil formation. Soil
Color. SSSA Special Publication No.
3 1 : 51-69.
Schwertmann, U, H. Kodama, and W. R. Fischer.
1986.Mutual interactions between
organics and iron oxides. In
:P. M. Huang and M. Schnitzer (eds.). Interactions
of Soil Minerals with Natural Organics and Microbes. SSSA Spec. Pub. No.
17: 223-250.Schwertmann, U. and R. M. Taylor,
1989.Iron oxides. In
:Dixon,
J . B , and S.
8.Weed
(eds.). Minerals in Soil Environments. SSSA. Madison, Wisconsin, USA, p.
379- 438.Sharma, P. K., and S. K. De Datta.
1985a.Effecs of puddling on soil physical properties
and processes
.
In:. Soil Physics and Rice. IRRI, Los Banos, Laguna, Philippines.
p. 217-234
Sharma, P. K., and S. K. De Datta.
1985b.Puddling influence on soil, rice development
and yield. Soil Sci. Soc.
Am.J.
49: 1451-1457.Shoji, S., M. Nanzyo and R. A. Dahlgren.
1993.Volcanic ash soils- Genesis, properties
and utilization. Elsevier, Amsterdam.
Shoji, S., M. Nanzyo, R. A. Dahtgren and P. Quantin.
1996.Evaluation and proposed
revisions of criteria for andosols in the word reference base for soil resources. Soil
Sci.
161: 604-615Shoji, S., S. Kobayashi, I.
Yarnada and
J.Masui.
1975.Chemical and mineralogical
studies on volcanic ashes: I. Chemical composition of volcanic ashes and their
classification. Soil Sci. Plant Nutr.
21
: 3 1 1-3 18.Shoji, S.,
T. Takahashi, T. Ito and C. L. Ping.
1988.Properties and classification of
selected volcanic ash soils from Kenai Peninsula, Alaska. Soil Sci.
145: 385-413.Simonson, R.
W.
1959.Outline of generalized theory of soils genesis. Soils Sci. Soc.
Am. Proc.
23: 152-156.Soepraptohardjo,
M.and
H.Suhardjo.
1978.Rice soils of Indonesia. In: Soil and Rice.
IRRI. Los
Banos,Laguna, PhiUippines. p.
99-1 14Soil Survey Division Staff.
1993.Soil Survey Manual. USDA Handbook No.
18.Soil Survey Staff. 1975. Soil Taxonomy. USDA. Agr. Handbook 436.
U.S. Govt.
Printing Office, Washington.
Soil Survey Staff. 1994.
Keys to Soil Taxonomy.
Sixth Edition.
USDA-Soil
Conservation Service. Washington DC
Soil Survey Staff. 1998. Keys to Soil Taxonomy. Eighth Edition, USDA-Natural
Resources Conservation Service. Washington DC.
Soil Survey Staff. 1999. Soil Taxonomy. USDA. Second Edition. Agr. Handbook 436.
USDA-Natural Resources Conservation Service. Washington DC.
Stoops, G. and H. Eswaran. 1985. Morphological characteristics of wet soils.
1 ~ 7 :Wetland Soils: Characterization. classification. and utilization.
IRRI.
Los Banos.
Laguna, Philliines,
p.177-206.
Supriyo, H., N. Matsue and N. Yoshinaga. 1992. Chemical and mineralogical properties
of volcanic ash soils from Java. Soil Sci. Plant Nutr. 38(3): 443-457
Sutanto, R. 1988. Mineralogy, charge properrties and classification of soils on volcanic
materials and limestone in Central Java (Indonesia). PhD-Thesis. RUG, Gent.
Swindale, L. D. 1965. The properties of soils derived from volcanic ash. Meeting on the
class. and corr. of soils from volcanic ash. FAO-Report Rome 14: 53-55
Tan, K. H. 1965. The andosols in Indonesia. Meeting on the class, and corr. of soils *om
volcanic ash. FAO-Report Rome 14: 30-3
5.Tan, K. H. 1968. The genesis and characteristics of paddy soil in Indonesia. Soil Sci.
Plant Nutr. 14(3): 1 17-121
Tan,
K. H. 1993. Principles of Soils Chemistry. 2nd ed. Marcel Dekker, Inc. New York.
362p.
Tan K. H. and J. van Schuylenborgh. 1959. On the classification and genesis
ofsoils
derivated e o m andesitic volcanic material under a monsoon climate. Neth.
J. of
Agric. Sci. 7: 1-21.
Tim Pusat Penelitian Tanah dan Agrokimat. 1994. Laporan
akhirsurvei dan pemetaan
sumberdaya lahan untuk pengembangan pertanian lahan kering dan konservasi
hutan Propinsi Daerah Istimewa Yogyakarta.
Bag. Proyek Pengelolaaan
Sumberdaya Tanah. Pusat Penelitian Tanah
dan
Agroklimat
USDA-NRCS. 1995. Soil survey laboratory information manual. National Soil Survey
Center. Soil Survey Laboratory Lincoln, Nebraska. Soil Survey Investigation
ReportNo. 45. Ver. 1.0.
Utarni, S. R. 1998. Properties and rational management aspects of volcanic ash soils from
Java, Indonesia. PhD-Thesis. RUG, Gent.
van Bemmelen, R.
W.1949. The Geology of Indonesia. Vol.lA. General Geology of
Indonesia and Adjacent Archipelagoes. Gov. Printing Off., The Haque, 732
p.van Breemen,
N.,P. Buurmann and R. Brinkman. 1992. Processes in soils. Text for
Course J050-202.
Dept Soil Science
&Geology, Agricultural University,
Wageningen. 202p
van Wambeke,
A.1985. Calculated Soil Moisture and Temperature Regimes of Asia.
SMSS Technical Monograph
#9.Soil Management Support Sevices, Soil
Conservation Service, USDA, Washington, DC. 144p
van Wambeke,
A.1992. Soils of the Tropics: Properties and Appraisal. McGraw-Hill,
Inc. New York.
Wada, K. 1980. Jkfineralogical characteristics of Andisols.
In: B. K. G. Theng (ed.). Soil
with variable charge. NZ Soc. Soil Sci. Lower Hutt, p. 83-107.
Wada, K. 1985. The distinctive properties of Andosols. In; Advances in Soil Science.
Vol. 2: 174-229
Wada, K. 1989. Allophane and imogolite.
In
:Dixon, J.B. and S.B. Weed (eds.)
Minerals in Soil Environments. SSSA. Madison, Wisconsin, USA. pp: 1051-1088.
Wada, H. and H.
U. Neue. 1988.
Chemistry and biochemistry of paddy soils.
Proceedings of the
9thInternational Soil Classification Workshop: Properties,
classification and Utilization of Andisol and Paddy Soils. Japan. p. 169-174
Wada, K. and M. E. Harward. 1974. Amorphous clay constituents of soils.
In;
Advances
in Agronomy. Vol. 26: 2 1 1-260
Walker,
A.L. 1983. The effects of magnetite on oxalate- and dithionite-extractable iron.
Soil Sci. SOC.
Am.J. 47: 1022-1026.
Wielemaker, W. G. and T. Wakatsuki. 1984. Properties, weathering and classification of
some soils formed in peralkaline volcanic ash in Kenya. Geoderma, 32: 21
-44.Wilson, M. J.
1987.X-ray powder diffraction methods.
In: Wilson, M.
J.(ed).
A
Handbook of Determinative Methods in Clay Mineralogy. Blackie. Glasgow and
London, p. 26-98.
Yamada,
I . ,H. Kubodera and S . Shoji.
1994.Indurated volcanic ash soils in Japan, their
characterization, land
use and management.
Irr
:Trans. 15th World Soil Science
Congress, Acapulco, Symposium
ID 13,The Indurated volcanic soils. 62:
487-LAMPIRAN
1.Contoh Perhitungan Regim
LengasTanah Menurut Program
Newhdl Simulation Model (NSM
c . ~ ~ . ,
..
,,.
t r i x n i s i ! :820 ma 7 . . . -. . .i rxiyrv .TU;E r ~ g i s r : I ~ ' ~ ! t y ~ e ~ ? h ~ r z i ~ M o i s t u r ~ r e g i a ~ : Udic
SCtL tilHATIC REGitlE 6CCOHDING TE NEUHALL CO~PUTGTIDt4
: r a i l t e s p . = a i r ? e s p . + 2 . 5 C; a m p l l t , reduced by i / 3 j
J6K FEB MAR RPR MAY JUN JUL AU6 SEP DCT NOV DEC
mon:hiy r a i n f a i i i m m l 4??,0 343.0 362.0 2Rb.0 167.0 1 1 5 . 0 4 1 . 0 43.0 9 2 . 0 139.0 344.0 385.0 monthly a i r t e c p e r a t u r e s (Ce!ciusl ? ? 2 1 . 2 23.2 27.4 23.0 20.4 2 2 . 2 1 7 . 4 21.0 19.8 2 0 . 2 20.3 2 1 . 0 teonthly e v a p o t r a n s p i r a t i o n ( T h o r n t h n a i t e ! . me. ?b,O R5.0 9 5 . 8 96.1 74.7 8 6 . 7 51.0 77.6 6 8 . 5 7 6 . 0 75.6 8 5 . 1 EOISIURE CGLENDhH I = d r y 1 2 = a/d ; 3 = m o i s t 3RN ""-"x'?xT' " 7 7 - 7 7 - " J > J J ~ > J ; J ; L . L ~ ~ J ~ J J ~ J J A J L ' ~ ~ ~ ~ ~ ~ FEB 3333'-' 7-"77' 23~3J3~~~Jd33;3:j333333333 MAR 333333353333333333333333333333 APR 3333333333333333333333j3333333 N R Y 333333333333333333333333333333 JUH 33333333333333333333333333353 JUL 333333333333333333333333333333 AU6 333333333333333333333333333333 SEP 33333333333333333333333333333 DEC 333333333333333333333333333333
:
h m b e r of c u e u l a t i v e d a y s t h a t:
H i g h e s t number cf c o n s e c u t i v e d a y s:
:
t h e m o i s t u r e c o n t r o l s e c t i o n:
t h a t t h e MCS i s...
:
During o n e y e a r: When s a i l temp
is:
Moist i n:
Drv:
f l o i s t:
is:
above 5 deg. C:
s o r e p a r t s : a f t e r suminer:after & i n t e r ::
DRY HiD NOIsT:
DRY M/o MOIST:
YEnR T>a:
S o l s t i ~ ~:
5 ~ 1 s t i c e :...
:
in 0 360 0o
360:
360 360:
it:
120:
e
Computed by BASIC program HSM, Noverber f9B6 T e n t a t i v e s u b d i v i s i o n : Typic Udic
LAMPIRAN
1.(Lanjutan)
T
Nusber o f cumulative d a y s t h a t:
Hxghest n u a b e r o f c o n s e c u t i v e days i:
t h e ~ a i s t u r e i ~ f i t r a i ~ e i t i o n:
t h a t t t ! ~ nts 1 s; During one year
:
#hen s o i l teap i s:
Hoist i n:
B r y i H o i s t:
. ~~3.5 ; above 5 deg. C I s o a e parts : a f t e r suffi8er:after winter:
; Y:D MOIST
:
DRY% / a
VdisT:
YEAR T)B:
a o i s t i c e:
~ a l r t i c e:
I
Cornputel ny BASIL program NSH. November 1986 7 e n t a t i ; e 5 u b d i v l S ~ U n : Typic Udlc
LAMPIRAN
1 .(Lanjutan)
month:! ; a l r f a I I ton,!
.?Z&.> y 1 . 0
"'
,..,.u " ' - i > 9 . $ i37.3 68.0 2 6 . 0 I3.0 7 7 . 8 . i.:5.0 - 2 i 5 . O 2:i.u acst!,:y s i r t e a p e r ~ t u r e s < C e i r i z s !i, ; h , j - . 2b.5 26.8 2 t . 3 16.1 25.5 2 5 . 4 2 6 . 7 2 i . 0
27.c 2 b . a
e o z l h i y eva?ctrarz;piieticn [ihornth*aitej, am.
??. 0 ..? ....,.
.
,..4.S iil.2 i 3 4 . 2 1;b.' 123.4 1 1 4 . 4 116.2 129.1 I e 2 . 5 i.19.' 14,s.: - ~ -%c!:Si~pE CALEWDAR i : d r i 1 2 = a i d 1 3 = ~ o i s l JGrJ 33333j33333333333333.j3.3333 j j3.3 J9L 3333335;333333333333j333333222 hue 22222222222222222222222222222: SEP 221flifii?ii1112?2222222222222 OCT 2illillili11i11222222222222222 NOV 2?22?2222222222333333333333333 DEE j333333333332333j3333333333333:
H u a t ~ r a f cumulative days that:
Hiqhest number o f consecutive d a j s I:
the ~ o i s t a r e control section ; that t h e HE5 is:
During one year 1 #hen s o i l tesp i s:
Boist i n:
Dry:
! k i s t:
1%
:
above 5 dea. C:
some p a r t s : a f t e r suamer:after winter::
DRY k!!J MGlST:
DRY k!D MOIST:
Y E A R T > 8 : ; o i s t i c e:
so is tic^:
...
:
26 82 252:
26 62 252 ; 317 317:
0 : 2 7 :*
Coaputed by BRSIC prograffi W H , Hove~Ser 1986 Tentative subdivision: IJdic Tropustic
LAMPIRAN
1.(Lanjutan)
s c n t R j . r;ifiia:l !!?cj
G < . f ' . i Z 5 . T . i 7;c.i ib".l t<,.; .?I,- 2 9 . 3 ti.; 12;': 1 9 . 2 ri:," - - " , 5 , - . . = . . .
; j n t ? i . v a:: t?eperat;iec (CeIrlos)
7 ; s ?GI: Z b . 5 2 6 . 9 2 7 . 6
r b . :
F C =. 2 5 1 5L 1 . r 2 0 . 5 L7.2
::.:
.
-b . ' *'
. .
noote;!y ev&p;transpirati;fi i?horfithrai:?i. sr.
i,:rs.c
i.21,: iqi.2 1 3 4 . 2 ji1.5 127.9 i l b . 6 i i i . 3 125.0 1 4 7 . 3 1 ~ 5 . 2 i L 6 . l f i G I S T U R i CALEt4SAR. _
. .
- _
;-
u i y.
- f / O : 2-
Z G i C I :AX =EB Mai: RF.R i(6Y.
, .*. ;s,i j ,li RGCi SEP OCT #U'J DEt3I Humhe- o: c u a u l s i i r e d a y s that
:
Highest nusber af r ~ n s r c u t i d e d i y s :I t;e n ~ i s t u r e r o n t r c i sectinn
:
.
~ ! i a t L-
the f?CS i r:
During one year:
Wnen r o i ! temp 1s:
Hoist in:
Dry:
noist:
.-
1 9
:
above 5 deg. C:
soae parts : d f i ~ r 5uaser:after inter: I W Y X i D NOIS: ; DRY EID HOIST:
YEfiR T > 6:
s o l s t i c e:
s o i s t i c e:
t
Complited by BRSIE: program K!4, Nnvenber iV8b Tentative subdivision: Udic Trapustic
Gambar
L2 I'ola
Dihksi Sinar-X
(XRD) Fraksi Liat padaKelompok
Tekstur A4d19er Pasir Berkerikil Elevasi 350 - 500 mdpl:
(a)Horison
BwlTYG-Gambar L3. Pola D i h k s i Sinar
-X
(XRD)
Fraksi Liat pada Kelompok~ekstur
Pasir, Elevasi 350-
500 m dpl: (a) Horison ZBqmlMG-12 (Lahan Kering); @), Horiscm ZBsdm/YG-10 (Sawah 1 x Padi); (c). Horison 2Bqm/YG-10 (Sawah I xPadi).
Gambar
L4.
Iyola
Dihksi Sinar-X
(XRD) Fraksi Liat pa&Kelompok
TeksturPasir,
I?Ievasi 350 - 500 m dpl, Pedon YG-I (2 x Padi); (a)
Horison
Apl; @)liorison
4 2 : (c)Horison
Bsdm.Gambar
LS.
IPola
Di-i Sinar-X(XRD)
Fraksi Liat padaKelompok
Tekstur Pasir,IElevasi
350-
500 m dpl, Pedm YG-2 (3 x Padi); (a)Horiscm
Ap; @)I-Iorisan
Ad
1 ; (c) HorisanBA
,.
. -Gambar
L6.
l'ola D W i Sinar-X
(XRD) Fraksi Liat pa& Kelompok Tekstw l ~ m p u n g Berpasir, Elevasi 350-
500rn
dpl: (a) Horison BANG-22 (Lahan Kering); @), Horison Bdm/YG-7 (Sawah 1 xPadi);
(c) Horison lMlYG-6 (Sawah 3 xPadi).
GambarL7. F'ola Difi-aksi Sinar-X (XRD) Fraksi Liat pada
Kelompok
Tekstur Lanpung BerpasirElevasi
<250 m dpl, PedonYG-17
(Sawah 3 x Padi);Gambar L8.
PoIa
Dil?aksi Sinar-X(XRD)
Fraksi Liat Pada 2 adari
25"- 50"
dari (a)HLorison
2Bqm/YG-10; (b)Horison
Bsdm/YG-7.Gambar L9. Kurva Analisis Beda Termal @TA) Fraksi Liat pada Kelompok Tekstur M'odrfier Pasir Berkerikil Elevasi 350 - 500 m
dpl:
(a) Horisan BAIYG-14@ahan
Kering);(b)
Horison BsdmJYG-4 (Sawah 1 x Padi); (c) Horison BUYG-13 (Sawah 3 x Padi).Gambar
L10.
Kurva Analisis Beda Termal (DTA) Fraksi Liat pada Kelompok Tekshu. PasirElevasi
350 - 500 m dpl. Pedaa YG-1(Sawah
2 x Padi): (a) Horiscm Apl; @) Horiscn Ap2; (c) Horiscm Bsdm.Gambar
L l l . Kurva Analisis Beda T e d@TA)
Fraksi Liat pa& Kelompok Tekstur Lempung Berpasir Elevasi 350-
500 m dpl: (a) HoriscmAB/YG-22 (Lahan Kering); (b) Horison Bsdm/YG-7 ( S a d 2 x
Padi);
LAMPIRAN
12.
Ikhtisar
Deskripsi Lingkungan Pedon di
Daerah
Penelitian
No.
1
Nomor PsdonlI
Elevasil ~ r
tanah1 Lueng %1
Vegetasil Pmgg. LahanI
CH, mmith1
Suhu rata-rata1
Regim1
TaksonomiI
Lokasi(
m, dplI
cm l ~ w a l l ~ i n i1
JenisI
Dominanl Pola1
Stasiun lklim1
~ d a r a l Tanah lengas Tanad Tanah (SSS, 1998)Tekstur
ModGerPasir Berkenlal (Elevasi 300
-
SO0
m
$1)
1 YG-141 Senbungan, Cangkringan 495 120 5 5 Pekaranw Duriin, Melinjau 28201 Pakem 21.0 23.5 Udk Typic Hapludolls 2 YGd! MKS, ~ . 2 k ??5 ??",'? ? 1 $$:.%h 4 " A *o*n, n -a,-- - 4 n
.,.,
r A,...:,ml Lurw rqnw11 C I . Y '4.4 MYIK AC~F EFquepi 3 YG-BIGrogolsai, Ngaglik 370 7200 2 1 Sawah 2x Padi 28201 Pakm 21.0 23.5 Akuik Aeric Epiaquept 4 YG-13 Wukirsai, Cangkringan 465 56 6 1 Sawah 3x Padi 28201 Pakem 21.0 23.5 Akuik Awic Epiaquept
I~ekstw
~ o d i f i e rPasir Berkaikil (Elevasi 4 5 0
rn
dpl)
13 YG211 Calukan, Ngaglik 245 >200 2 2 Pekmngan Kelapg, ma@ 19421 Ngaglik 24.9 27.4 Udik Typic Hapludoll 14 YG-2W Calukan, Nqsglik 240 ?2W 3 1 Sawah 1x Padi 19421 Ngaglik 24.9 27.4 Akuik Aeric Epiaquept
Tekstur Pasir (Elevasi 300
-
500
m
$1)5 YG-121 Kaliwanglu, Pakem 360 >ZOO 4 4 Pekmngan Melinjau, kelapa 28201 Pakem 21.0 23.5 Udik Typic Hapludoll 6 YG-101 Kaliwanglu, Pakem 340 ,200 3 1 Sawah l x Padi 28201 Pakem 21.0 23.5 Akuik Aquic Durudept 7 YG-lIKaliwanglu, Pakm 350 ,200 3 1 Sawah 2x Padi 28201Pakem 21.0 23.5 Udik Anthraquic Euhdept 8 YG-21Kaliwangfu. Pakem 345 150 4 1 Sawah 3x Padi 28201 Pakem 21.0 23.5 Akuik Typic Epiaquept
Tekstur Pasir (Elevasi Q50
mdpl)
15 YG.161 Mudal, Ngaglik 200 120 2 2 Peka'anpn Barnbu, kelapa 19421 Ngagllk 24.9 27.4 Udik Typic Hapludoll 16 YG-191 Mdal, Nmlik 205 >200 2 1 Sawah 1Rx Padi 19421 Ngqlik 24.9 27.4 Akuik Anthraquic Eubudept
-
Tekstur
h p u n gBepasir (Elevasi 300
-
500
m
dpl)
9 YG-22lKembangaum, Turi 390 >200 5 5 Kebunl Pek Salak 31921Turi 23.2 25.7 Udik Andic Hapludoll 10 YE71
W L w ,
Ngaglik330
105 2 1 Sawah I x Pa& 31921 Turi 23.2 25.7 Akuik F r q c Epiaquept 11 Y G 8 Ngepos-lor, Ngaglik340
115 1 Sawah 2x Padi 31921 Turi 23.2 25.7 Akuik F q i c Epiaquept 12 YG-61 Ngepas-lw, Ngaglik 315 72 5 1 Sawdh 3x Padi 31921 Tun 23.2 25.7 Akuik Typic EpiaqueptTekstur
Lempung Pasir (Elevasi 4 5 0m
dpl)
17 YG.IBICokIwrijayan, Gaping 110 ,200 2 2 Peka'angan Bambu, kelapa 20971 UGM 26.4 28.9 Ustik Typic Haplustoll 18 Y W Trini, Gmping 140 >2W 3 1 Samh
ix
Padi 20971 UGM 26.4 28.9 Akuik Fragic Epiaquept 19 Y G . 1 7 1 N ~ n . Gaping 160 72M) 3 1 Sawah3x Padi
20971 UGM 26.4 28.9 Akuik Typic EpiaqueptLAMPRAN
1 3 .Deskripsi Profil Tanah Daerah Penelitian
PEDON : YG-1DAERAH : Yog yakarta
LOKASI : 10 meter ke arah barat dari pertigaan jalan Kaliwanglu dan Kaliwanglu-Pakem, Desa Harjobi~nangun. Kec. Pakem, Kab. Sleman, kurang-lebih 7°40'45" LS dan 110° 24' 13" BT.
FlSlOGRAFl : 1-ereng bawah volkan
KARAKTERISTIK LERENG : Teras (sawah)
ELEVASI :
-
3510 m. dm1CURAH HUJAN : 1806 mmRahun (Ngemplak); 4 bulan kering dan 5 bulan basah
KEDALAMAN hdUKA AIR TANAH : 22 meter
DRAINASE : Agak terhambat
PERMEABIUTAS : Lambat
PENGGUNAAFI LAHAN : Sawah 2x Padi
IRlGASl : Sedemana
BAHAN INDUK : Bahan volkan dari Gunung Merapi
KLASIFIKASI : Anthraquic Eutmdept, berlempung kasar, campuran, isohipertermik HORISON PENClRl : Okrik
-
KambikPENGAMBllAbl CONTOH : Tanggal: 28 Oktober 1997
Apl-- 0
--
15 cm; kelabu muda kewklatan (lOYR612) kering; coklat tua (10YR3/3) lembab; pasir bt!rlempung; struktur granuler; gumpat membulat halus lemah; gembur (lembab). agak lekat tidak plastis (basah); pori-pori halus, sedang. kasar cukup; perakaran halus, sedang banyak; batas jelas rataAp2
--
15-
23 cm; kelabu muda kewklatan (10YR612) kering; kelabu sangat tua (10YR311) Iembab lempung berpasir; karatan besi coklat kuat (7.5YR5/6) ) jelas sedang, cukup; stmktur gumpal membulat halus lemah-
sedang; gembur (Iembab), agak lekat tidak plastis (basah); pori-pori halus, sedang, kasar cukup; perakaran halus, sedang banyak; batas jelas rataBsdm
--
23-
31 cm; kelabu muda (10YR712) kering; coklat sangat tua kekelabuan (10YR312) lembab, pasir beriempung; karatan besi doklat kuat (7.5YR5/6) jelas sedang, sangat banyak, membentuk garis setebal 1 cm, karatan Mn hitam (10YR211) jelas, sedang. cukup; struktur gumpal membulat. halus, lemah-
agak masip. sangat teguh sekali (lembat~). tidak lekat. tidak plastis (basah); pori-pori halus, sedikit sekali; perakaran halus. sediki sekali; batas jelas rataB w l
-
31-
45 cm; kelabu muda (10YR7/2) kering; cokfat sangat tua kekelabuan (10YR3/2) lembab; pasir berlempung; s t ~ k t u r gumpal membulat halus lemah; gembur (lembab). tidak lekat, tidak plastis (basah); pori-pori halus, sedang, kasar cukup; perakaran halus, sedang sedikit; batas jelas rataBw2
-
45-
85 tm; keIabu muda (10YR712) kering; coklat tua kekelabuan (10YR3/2) lembab; pasir berlempung; s t ~ k t u r gumpal membulat halus lemah; agak gembur (lembab), t i i a k lekat, tidak plastis (basah); pori-pori halus, sedang. kasar cukup; perakaran halus, sedikii; lbatas jelas rata2Bw3
-
85-
91 cm; wklat tua kekuningan (fOYR3/4) lembab; pasir berlempung; struktur gumpal membulat halus lemah; gembur (lembab), tidak lekat. tidak plastis (basah); pori- pori hal~ls, sedang. kasar banyak; perakaran halus sedikit; batas jelas rata2Bw4
-
91-
1.14 c m ; coklat (10YR4M) iembab; pasir beriempung; sedikii berkerikil; masif; teguh ({trmbab). pori-pori halus, sedikit; perakaran halus sedikit; batas jelas rata2-5
-
114-
1 31 cm; coklat (10YR4/3) lembab; pasir berlempung; stmktur gumpal membulat halus lemah; gembur (lembab), tidak lekat, t i i a k plastis (basah); pori-pori halus, sedikii; perakarian halus sedikit; batas jelas rata2Bw6
--
131-
140 cm; coklat tua (10YR313) lembab; pasir berlempung; struktur gurnpal membulat halus lemah; gembur (lembab). agak keras, tidak lekat. tidak plastis (basah); pori-pol? halus. sedikit; perakaran halus sedikit; batas jelas rata2Bsdrnb
--
1 4 C l-
152 cm; coklat tua (10YR313) lembab; pasir berlempung; karatan Fe(10YR518). baur, kecil, sedikit; stmktur masif, sangat keras (lembab), pori-pori halus, sedikit; perakaran halus sangat sedikit; batas jelas rata
2Bwb
--
152-
163 cm; kelabu sangat tua (10YR3/1) lembab; pasir berlempung; stnrktur gumpal membulat halus lemah; gembur (lembab). tidak lekat, tidak plastis (basah); pori- pori halus, sedang, cukup; perakaran halus sangat sedikit; batas jetas rata3C'l
--
163-
181 cm; kelabu tua (10YR411) lembab; pasir {kasar); agak berkerikil; tidak berstmlrtur (lepas); gembur (lembab). tidak lekat. tidak plastis (basah); pori-pori halus. sedikit; perakaran halus sedikit; batae jelas rata4C2
-
181-
(i210) cm; kelabu tua (10YR4/1) lembab; pasir (halus); agak berkerikil; tidak berstmlrtur (lepas); gembur (lembab). tidak lekat. tidak plastis (basah); pori-pori halus. sedikii; perakaran tidak ada.LAMPIRAN
1:).(Lanjutan)
PEDON : YG-2DAERAH : Yogy,akarta
LOKASl : 25 mc?ter ke arah barat dari peltigaan jalan Kaliwanglu dan Kaliwanglu-Pakem, Desa Harjobinangun, Kec. Pakern. Kab. Sleman, kurang-Iebih 7O40'48" LS dan 110 24' 1 2
BT
- .
F1SIOGRAFt : Caerah depresi dari Lereng bawah volkan KARAKTERlSTlK LERENG : Teras (sawah)
EtEVASl : 340
In.
dm1CURAH HUJAN : 1806 mmltahun (Ngemplak); 4 bufan kering dan 5 bulan basah KEDALAMAN MUKA AIR TANAH : 150 cm
DRAINASE : Te~hambat
PERMEABILITAS : Lambat
PENGGUNAAN LAHAN : Sawah 3x Padi
IRlGASl : Sedeihana
BAHAN INDUK : Bahan volkan dari Gunung Merapi
KLASlFlKASl : Typic Epiaquept. berlempung kasar, campuran, aktif. tidak masam, isohiper- terrnik
HORISON PENCIRI : Okrik
-
KambikPENGAMBILAN CONTOH TANGGAL: 29 OktOber 1997
Ap
-
0-
16 cni; Coklat tua (10YR3/3) lembab; lempung berpasir; karatan besi. coklat kuat (7.5YR416:1 jelas, cukup, sedang; stnlktur gumpal membulat sedang halus: gembur (lembab). agak lekat. agak plastis (basah); pori-pori halus, sedang, kasar cukup; perakaran halus, sed;ang banyak; batas jelas rataAd
-
16-
22 Cni; coklat sangat tua kekelabuan (10YR3/2) lembab; pasir berlempung; karatan besi coklilt kuat (7.5YR4/6) jelas, sedang. banyak. karatan Mn hitam (10 YR2/1) jelas. halus, sedikit; stmktur gumpal membulat halus lemah; agak teguh (lembab). agak lekat tidak plastis (basah); pori-pori halus, sedikit; perakaran tidak ada; batas jelas rataBA
--
22-
34 cni; coklat sangat tua kekelabuan (10YR312) lembab; pasir berlempung, karatan besi coktat kuat (7.5YR5/6), jelas, halus, sedikit. karatan Mn hitarn (10YR2/1). jelas, halus. sedikit; struktur gumpal membulat halus lemah; agak teguh (lembab), agak lekat tidak plastis (basah); pori-pori halus;sedang, kasar cukup; perakaran tidak ada; batas jelas rata batas jelas rataBw
-
34-
69 WI; kelabu sangat tua (-lOYR3/1) lembab; lempung berpasir; karatan besi coklat kuat (7.5YR4B) jelas. halus, cukup; struktur gumpal membulat sedang-cukup; gembur (lernbab). iagak lekat tidak plastis (basah); pori-pori halus, sedang, Icasar cukup; perakaran tidak ada; batas jelas rataB g l
-
69-
110 cm; kelabu sangat tua (1 0YR3/1) lembab; pasir berlempung; karatan besi coklat kuat (7.5YR5/6), jelas, sedikii. halus; ~ t ~ k t u r gumpal membutat sedang-lemah; gembur (lembab), ltidak lekat, tidak plastis (basah); pori-pori halus, sedang; perakaran tidak ada; batas jelas rata.Bg2 -110
-
145 cm; kelabu sangat tua (10YR311) lembab; pasir berlempung; s t ~ k t u r gumpal membulat sedang-lemah; gembur (lembab). tidak lekat, tidak plastis (basah); pori-pori halus, sedilng; perakaran tidak ada; batas jelas rata.2Cg3
-
s145cm
:
kelabu sangat tua (10YR3/t) lembab; pasir; tidak berstruktur (butir tunggai). pori halus, sedang kasar cukup.222
LAM~IRAN
L
3.
(Lmjutm)
PEDON : YG-:)
DAERAH : Yojlyakarta
LOKASl : 20CI rn arah selatan perernpatan yang rnengubungkan jalan lingkar utara dengan ibukotil Kecamatan Gamping, Dukuh Trini. Desa Trihanggo. Kec. Garnping, Kab. Slernan, kurang-lebih 7044'58" LS dan 11 0 20' 46" BT
FtSlOGRAFl : Dataran volkan
KARAKTERIS'TIK LERENG : Teras (sawah) ELEVASI : 14CI rn. drnl
CURAH HUJAN : 2097 rnrnnahun (LJGM); .5. bulan kering dan .5. bulan basah
KEDALAMAN MUKA AIR TANAH :
-
crnORAINASE : Sangat larnbat PERMEABILITAS : Larnbat
PENGGUNAAIV LAHAN : Sawah 2x Padi IRlGASl : Sederhana
BAHAN INDUP: : Bahan volkan dari Gunung Merapi
KLASlFlKASl Fragic Epiaquept. berlernpung kasar, carnpuran, aktif, tidak masam. isohiper- termik
HORISON PEIKXRI : Okrik
-
KambikPENGAMBILAN CONTOH TANGGAL: 19 Desember 1997
Ap
-
0--
12 crn; Coklat sangat tua kekelabuan (10YR312) lembab; lempung berpasir; karatan besi. coklat (7.5YR414) nyata. sedikit, kecil; struktur butir. sedang, cukup; gernbur (lernbab), agak lekat. agak plastis (basah); pori-pori halus dan sedang, banyak, kasar sedikii; akar halus banyak, sedang biasa; batas nyata rataf3d
-
12-
32 cm; coklat tua (10YR313) lernbab; lernpung berpasir; karatan besi coklat tua kernerahan (5YR3/4) nyata, kecil, biasa; struktur gumpal rnernbulat sedang-cukup; agak teguh-
leguh (lernbab), agak lekat tidak plastis (basah); pori-pori halus, sedang. kasar, sediki; perakaran halus sedikit; batas jelas rataB w l
-
32-
45 cm; coklat sangat tua kekelabuan (10YR3/2) lembab; lernpung berpasir, karatan besi coklat tua kernerahan (5YR314). jelas, kasar, banyak; struMur gumpal mernbutat. Sedan9 ~:ukup; agak teguh (lembab). agak lekat tidak plastis (basah); pori-pori halus. sedang, Icasar sediki akar halus sedikii; batas jelas rata2Bw2
--
45-
5 4 cm; coklat tua kekelabuan (10YR4/2) lembab; lempung berpasir; karatan besi coklat tua kernerahan (5YR3/3) nyata. kasar, sediki; struktur gumpal rnernbulat halus- lernah; gembur (lembab), tidak lekat t i i a k plastis (basah); pod-pori halus biasa. sedang, kasar cukup; perakaran tidak ada; batas jelas rata2Bsdrnb
-
54-
75 c m ; coklat tua <lOYR4/3) lernbab; lempung berpasir; karatan mangan coklat sangat tcla (10YR2/2). nyata. banyak, sedang; struktur gumpal rnernbulat halussedang lernah; sangat teguh (lembab). tidak lekat, t i i a k plastis (basah); pori-pori halus, sedang. kasar setlikit; perakaran tidak ada; batas jelas rata.2 M l -75
-
100 crn; coklat tua kekuningan (10YR3/4) lembab; lernpung liat berpasir; karatan mangan coklat sangat tua (tOYR212). jelas.biasa, kasar; S t ~ M u r gumpal membulat sedang-Iemah; agak-teguh (lembab). t i i a k lekat. tidak plastis (basah); pori-pori halus. sedang biasa, kasar banyak; perakaran tidak ada; batas jelas rata.2Bwb2
-
100-
128 cm; coklat sangat tua kekelabuan (10YR3E) lernbab; lempung; karatanmangan hitam (5YR2.5/1), baur, biasa, kasar; stmktur gumpal bersudut, sedang cukup. agak teguh, agak lekat agak plastis pori halus seikii, sedang kasar biasa; batas jetas rata 2 M 3
-
128-
(210) cm; coklat tua kekuningan (10YR3/4) lembab; lernpung berpasir; karatanmangan hitam (5YR2.511). baur biasa kasar; struMur gumpal rnernbulat, sedang cukup. agak t e g ~ ~ h . agak lekat agak plastis; pori hatus sedikit, sedang kasar biasa
LAMPIRAN
13. (~anjutanjPEDON : YG-4 DAERAH : Yoglyakarta
LOKASI : 50 N I arah utara timur laut pertigaan jalan Ngemplak
-
Dukuh Meces. Desa Umbul- martani. Kec. Ngemplak. Kab. Sleman, kurang-lebih 7O40'36" LS dan 110° 25' 29" BT FISIOGRAFI : Lereng bawah volkanKARAKTERISTIK LERENG : Teras (sawah) ELEVASf : 375 m. dml
CURAH HUJAhl : 2820 mmnahun (Pakern); 3 bulan kering dan 6 butan basah
KEDALAMAN klUKA AIR TANAH :
--
cmDRAINASE : Limbat
PERMEABILITAS : Agak Lambat
PENGGUNAAN LAHAN : Sawah. 1 kali padi IRlGASl : Sedesrhana
BAHAN INDUK : Bahan volkan dari Gunung Merapi
KUSlFlKASl : Aeric Epiaquept, berlempung kasar di atas skeletal berpasir, campuran, superaktif, tidak masam, isohipertermik
HORlSON PENClRl : Okrik
-
KambikPENGAMBllAhl CONTOH TANGGAL: 20 Desember 1997
A p l
--
0--
14, cm; wklat sangat tua (10YR212) lembab; kelabu rnuda (10YR712) kering; lempung Iberpasir; struktur butir sedang cukup; gembur (lembab), agak lekat, agak plastis (basah); (~ori-pori halus. sedang. kasar banyak; perakaran halus. sedang banyak; batas jelas rataAp2
--
14-
20 tm; wklat sangat fua kekelabuan (10YR312) lembab; lempung berpasir, karatan besi wklat (7.5YR414) baur, kecil, sedikit; stmktur gumpal rnembulat sedang cukup; gembur (lembab). agak tekat agak plastis (basah); pori-pori halus, sedang kasar banyak; perakaran halus sedikii; batas jelas rataBsdm
-
20-
:31 cm; wklat tua (10YR313) lembab; lempung berpasir, karatan besi wklat (7.5YR4/4), nyata, sedang. banyak; struktur gumpal rnembulat halus lemah; teguh (lembab). tidak lekat tidak plastis (basah); pori-pori haius. sedang, kasar sedikii; perakaran tidak ada; batas jelas rataB w l
-
31-
43 cm; coklat kelabu sangat tua (lOYR3/2) lembab; lempung berpasir; karatan besi wklat tua kemerahan (5YR312) jelas, kasar. banyak; ~ t ~ k t u r gumpal membulat sedang- lemah; agfak teguh (lembab), tidak lekat tidak plastis (basah); pori-pori halus, sedang, kasar biasa; perakaran tidak ada; batas jelas rata2C1
-
43-
90 cm; w k l a i tua (10YR313) lembab; pasir berlempung; berkerikil 80% ukuran 2-
4 cm; karatran mangan coklat tua kemerahan (5YR3/2). baur. biasa. sedang; butir tunggal; sangat t q l u h (lembab). t i i a k lekat, tidak plastis (basah); pori-pori halus, sedang kasar, sedikit; perakafan tidak ada; batas jetas rata.2C2 -90
-
114 cm; coklat tua (10YR3/3) lembab; pasir berlempung berkerikil 90% ukuran 6-8 cm; karatan rnangan coMat tua kemerahan (5YR312). baur, biasa. sedang; strukturgumpal membulat halus-lemah; teguh (lernbab), t i i a k lekat, t i i a k plastis (basah); pori-pod halus, sedang sedikit; perakaran tidak ada; batas jelas rata.
3C3
-
114-
(17'5) c m ; coklat sangat tua kekelabuan (10YR312) lembab; pasir berlernpung; berkerikil 10% ukuran 3-
5 mm; karatan mangan coklat tua kemerahan (5YR3/2), baur. biasa, sedang; tidak berstruktur (butir tunggal), pori halus, sedang kasar biasa.LAMPIRAN 1 3 .
(Lanjutan)
PEDON : YG-5DAERAH : Yoglrakarta
LOKASl : 100 rn arah utara perernpatan yang mengubungkan jalan Belong
-
Gondang dan Jetis s u ~ h - Kadilobo. Dukuh Jetissu~h. Desa Donohajo. Kec. Ngagfik. Kab. Sleman; kurang-lebih 7O40'27" LS dan 1 10° 22' 44" BTFlSlOGRAFl : I-ereng bawah volkan KARAKTERtSTlK LERENG : Teras (sawah) ELEVASI : 340 rn. dm1
CURAH HUJAN : 3192 mmltahun
Vuri
); 2 bulan kering dan 8 butan basah KEDALAMAN NIUKA AIR TANAH : 11 5 cmDRAINASE : Lirmbat
PERMEABiLITAS : Agak Lambat
PENGGUNAAN LAHAN : Sawah, 1 kali padi IRIGASI : Sederhana
BAHAN INDUK : Bahan volkan dari Gunung Merapi
KLASIFIKASI : Fragic Epiaquept, berlempung kasar, campuran. superaktif. tidak-masam.
isnhimrfennik
.
- -
. . .-
.- -
. . .HORISON PEN'CIRI : Okrik- Karnbik
PENGAMBtLAhl CONTOH TANGGAL: 21 Desernber 1997
Apl
--
0--
12 c:m; coklat sangat tua-
kekelabuan (10YR312) lembab; lempung; struktur butir sedang CLI~UP; gembur (iembab), agak lekat. agak plastis (basah); pori-pori halus. sedang. kasar banyak; perakaran halus banyak. sedang biasa; batas baur rataAp2
--
12-
27 cm; coklat sangat tua kekelabuan (lOYR312) lembab; lempung; karatan besimerah-tua~ (2.5YR316) baur. sedang, biasa; struktur gumpal beffiudut sedang cukup; gembur (lembab). agak lekat agak plastis (basah); pori-pori halus, sedang banyak, kasar biasa; perakaran halus banyak; batas jelas rata
Bsdm
-
27-
40 crn; cokiat sangat tua kekelabuan (10YR312) lembab; lempung berpasir; karatan besi merah-tua (2.5YR316). nyata, kasar, biasa; struktur gumpal bersudut sednag lemah; teguh (lernbab), agak lekat tidak plastis (basah); pori-pori halus, sedang. kasar sedikii; perakaran halus sedikit; batas jelas rataBwl
-
40.- 54 cm; coklat tua (10YR3/3) lembab; pasir berlempung; karatan besi merah kekuningan (5YR4I6) baur, kecil, sedikit; struktur gumpal membulat sedang-lemah-
cukup; gembur (lembab). agak lekat tidak ptastis (basah); pori-pori halus, sedang, kasar biasa; perakaran tidak ada; batas baur rataBw2
-
54-
70 cm; coklat sangat tua kekelabuan (10YR3/2) lembab; lempung; karatan besi merah kekuningan (5YR4/0), nyata, kasar, biasa; gumpal-membulat sedang cukup; gernbur (Iembab), agak lekat. tidak plastis (basah); pori-pori halus, sedang banyak, kasar biasa; pecnkaran tidak ada; batas nyata berombak2Bsdmb -70
-
98 cm; coklat tua (10YR3/3) lembab; lempung berpasir; karatan besi merah kekuningan (5YR4/0), nyata. kasar, banyak; struktur gumpal rnembutat sedang-lemah; agak tegu~h (lembab), tidak lekat. tidak plastis (basah); pori-pori halus. sedang. kasar sedikit; perakaran tidak ada; batas nyata rata2C1
--
96-
118 cm ; coklat tua (lOYR313) lernbab; pasir berlernpung; berkerikil 10-
15% ukuran 3-
5 mm dan 3 cm; karatan mangan merah kotor (2.5YR312). jetas. banyak, kasar; struktur gt~mpal membulat sedang lemah-cukup; pori halus, sedang banyak, perakaran tidak ada; batas baur rata2C2
--
118-
155 cm ; coklat tua (10YR313) lembab; pasir berlempung; berkerikil 25% ukuran 2 cm; karat.an mangan merah kotor (2.5YR3/2), jelas, banyak, kasar; s t ~ k t u r gumpal membulat sedang lemah-cukup; pori halus, sedang banyak. perakaran tidak ada; batas jelas rata.-35C
-
155-
(1i30) cm ; coklat sangat tua kekelabuan (1OYR312) lembab; lempung berliat; struktur g~lmpal membulat sedang lemah-cukup; pori halus, sedang biasa, perakaran tidak ada.225
LAMPIRAN
'1 3. (Lanjutan)PEDON : YG-6
DAERAH : Yogyakarta
LOKASI : 50 m arah selatan tikungan tajam jalan Bafong
-
Gondang, Dukuh Ngepas Lor, Desa Donohi~rjo. Kec. Ngaglik, Kab. Sleman. kurang-lebih 7O40.35" LS dan 110 22' 3 0 BT FlSlOGRAFl : Lereng bawah volkanKARAKTERISl'IK LERENG : Teras (sawah) ELEVASI : 315 rn. dml
CURAH HUJAPl: 3192 rnmahun (Tun); 2 bulan kering dan 8 bulan basah
KEDALAMAN lllUKA AIR TANAH : 72 cm
DRAINASE : Lambat PERMEAB~LITI~S r Lambat
PENGGUNAAbl LAHAN : Sawah, 3 kali padi IRlGASl : Sed~trhana
BAHAN INDUK : Bahan volkan dari Gunung Merapi
KLASlFlKASl Aeric Epiaquept, berlempung kasar, campuran. superaktif, tidak rnasam. isohiperterrnik.
HORISON PEhlClRl : Okrik
-
KambikPENGAMBILAPJ CONTOH TANGGAL: 23 Desernber 1997
A p l
--
0-
15 cm; coklat sangat tua kekelabuan (10YR312) lembab; Iernpung berpasir; karatan besi merarh tua (2.5YR316). jelas, kecil, sedikii; s t ~ M u r gumpal membulat sedang wkup; gembur (llembab), agak lekat, agak plastis (basah); pan-pori halus, sedang, kasar banyak; perakaran halus sedang banyak. batas baur rataAp2
--
15-
25 Icm; coklat sangat tua kekelabuan (10YR3/2) lembab; ternpung berpasir; karatan besi melah-tua (2.5YR3/6) jelas, kecil. biasa; stmktur gurnpal mernbulat sedang cukup; gembur (llembab). agak lekat agak plastis (basah); pori-pori halus, banyak, sedang, kasar sedikit; pc!rakaran halus sedang banyak; batas jelas rataBd
-
25-
44 cni; coklat sangat tua (10YR212) lembab; lernpung berpasir; karatan besi merah-tua (2.5YR3fii). nyata. sedang, biasa; struktur gumpal bersudut sedang wkup; agak teguh (lembab). agak lekat agak plastis (basah); pori-pori halus. sedang, kasar sedikit; perakaran halus sedikit; batas nyata rata2Bxlmb
-
44-
55 cm; coklat sangat tua kekelabuan (10YR3/2) lembab; lempung berpasir;karatan tesi rnerah tua (2.5YR3B) nyata, sedang, banyak; struktur gurnpal rnembulat sedang-h.alus, lemah; teguh (lembab), t i i a k lekat tidak plastis (basah); pori-pori halus. sedang, kasar sediki; perakaran tidak ada; batas baur rata
2Bwbl
-
55-
67 crn; coklat sangat tua (lOYR2/2) lernbab; lempung berpasir, sangat berkerikil (30%0 diiirneter 4 mrn; karatan mangan merah kotor (2.5YR3/2), jelas. sedang. banyak; gurnpal-nbembulat halus wkup; agak teguh (lembab). t i i a k lekat, t i i a k plastis (basah); pori-pori tbalus, sedang sedikii; perakaran tidak ada; batas nyata berornbak2Bwb2 - 4 7
-
77 cm; coklat tua (10YR313) lernbab; pasir berlempung; karatan mangan rnerah kotor (2.5YR312). nyata, kasar, banyak; struktur gumpal rnembulat sedang-lemah; teguh (lembab), tidak lekat, tidak plastis (basah); pori-pori halus, sedang. sedikii; perakaran t i i a k ada; batas jefas berornbak2BC