DAFTAR PUSTAKA
Aleksandrova, L. N. 1967. Organomineral humic acid derivatives and methods of studying them. Paper read at a confrence on methods of studying humus. Commising I1of the All-Union Society of Scientist, February, 1967. Alloway, 6.J. and 0.C. Ayres. 1997. Chemical Principles of Environmnet Pollution. 2"d ed. Blackie Academic & Professional. pp. 66-85. Andriesse, 3. P. 1974. Tropical Peats in South East Asia. Department of Agriculture Research of the Royal Tropical Institute. Communication 63. Amsterdam. 63 p.
. 1988. Nature and management of tropical peat soil. F A 0 soils Bullet~n 5:s. Roma. . 1992. Constraints and opportunities for alternative use options of tropical peatlands. pp: 1-6. In: Tropica Peat, Proceeding of the International Symposium on Tropical peatlands. MARDI, Malaysia. Beroya, M. A. 2000. Mengenal Lingkungan Hidup : Pedoman Untuk Memperkuat Rakyat. Yakoma-PGI. Birkeland, P.W. 1974. Pedology, Weathering, and Geomorphological Research. Oxford Univ. Press. New York-London-Toronto. 285p. Boer, R., I. Nasution., I.Las dan A. Bey. 1996. Emisi metan dari lahan gambut sejuta hektar Kalimantan Tengah. Jurnal Agromet Vol. XI1 No. 1 dan 2, 1996/1997. pp. 31-38. Ebuwman, A. F. 1989. The role of soils and land use in the greenhouse effect. Netherlands Journal of Agriculture Science, 37 : 13-19.
. 1990. Exchange of greenhouse gasses between teresteriaf ecosystems and the atmosphere. Pp. 75-97. In A. F. Bouwman (Ed.). Sopil and the greenhouse effects.John Willey and Sons, Chichester. Brady, N.C. 1990. The Nature and Properties of Soils. The Mac Millan Co. New York. 653p. 1994. Effects of physical, chemical and Buttler, A., Dinel, H., and Leverque, P.E.M. botanical characteristics of peat on carbon gas flux. Soil Su. 158:365-374.
Chambers, M. 3. 1979. Rate of peat loss on the Upang transmigration projects, South Sumatera. Proc. Simp. Nas. I I I .Pengembangan Daerah Pasang Surut di Indonesia, pp. 765 777.
-
Cristenson, D.R. 1982. Lime, lime material and other soil amandemenh. pp. 331-348. In: V.C. Kilmer (ed). Handbook of Soil and Climate in Agriculture. CRC Press Inc. Boca Ratoon. New Delhi. Daubenmire, R. F. 1959. Plant and Environment. 2* ed. John Wiley & Sons Inc. New York. De Datta, K. 1981. Principles and Practices of Rice Production. John Wiley and Sons, Inc. New York. 618 p. Denier van der Gon, H.A.C. 1996. Methane emission from wetland rice fields. Doctoral Thesis. Agricultural University Wageningen. The Netherlands. Dickens, S. 1955. Recent experimental result on the trace element content of basic slag and blast furnace slag. Phosphosource. 15 : 251-260. Driessen, P.M. 1978. Peat soils. pp: 763-769. banos. Philippines.
In IRRI. Soil and Rice. IRRI. Los
Driessen, P.M. and M. Soepraptohardjo. 1974. Soil agricultural expansion in Indonesia. Bull. 1 : 1-63. Soil Res. Inst. Bogor. FAO-Unesco. 1974. Soil Map of the World. Vol. I. Legend. Unexo, Pans. flaig, W., H. Beuteelspacher and E. Rietz. 1975. Chemical composition and physical properties of humic substances, pp. 1-211. In 3.E. Gieseking, ed. Soil Component, Vol. I. Spriger-Verlag. New York. Halim, A. 1987. Pengaruh pencampuran tanah mineral dan basa dengan tanah gambut pedalaman Kalirnantan Tengah dalam budidaya tanaman kedelai. Disertasi Fakultas Pascasarjana, IPB. Bogor. 322 p. Hardjowigeno, S. 1993. Jakarta. 274 p.
Klasifikasi Tanah dan Pedogenesis. Akademika Pressindo.
.
19%. Pengembangan Lahan Gambut Untuk Pertanian : Suatu pefuang dan tantangan. Omsi Ilrniah Guru Besar Tetap Ilmu Tanah. Fakultas Pet-tijnian, IPB. 22 Juni 19%.
.
1997. Pemanfaatan gambut berwawasan lingkungan. Majalah Alami vol. 2 No. 1.Tahun 1997.
. 1998. Klasifikasi Tanah Garnbut. Jurusan Tanah. Fakultas Pertanian. Institut Pertanian Bogor. Hartley. R. D. and 0. C. Whitehead. 1985. Phenolic acids in soils and their influence on plant growth and soil microbial process. Pp 109-149. In Soil Organic Matter and Biological Activity. Developments in plant and soil Sciences Vol. 16 Mamunus Nijhoff/DR W. Junk Publisher. Dordrecht, Netherland. Institut Pertanian Bogor. 1980. Survai dan Pemetaan Tanah Daerah Air Padang - Air Sugihan Sub W S Sumatera Selatan. Proyek Pembukaan Persawahaan Pasang Surut (P4S). Ditjen Pangairan Dep. Pekei-jaan Umum dan Tenaga Listrik Inmtut Pertanian Bogor.
-
IPCC. 1990. Climate Change: The IPCC Scientific Assesment. Cambridge Univ. Press. Ismunadji, M. and G. Soepardi. 1984. Peat soils and crop production. Pp:488-502 In : IRRI. Organic Matter and Rice. IRRI. Los Banos. Philippines. Kanapathy, K. 1972. Copper requirement and residual effect with maize on a peat soil. Mal. Agric. 3. 48 : 249-263.
.
1975. Factors in the utilization of peat soil in Penisular Malaysia. Proc. 3& Asean Soil Cod. Kuala Lumpur. pp: 425432. Kantor Menteri Negara Lingkungan Hidup. 1999. Indonesia: The First National Communication. Under the United Nation Framework Convention on Climate change. State Ministry for Environment Republic of Indonesia. Jakarta, Oktober 1999. Kato, N. dan N. Owa. 1996. Dissoiution of slag fetiilizer in paddy soil and Si uptake by rice plant. Soil Sci. Plant Nutr. 43 : 329-341 Koswara, 0. 1985. Masalah-masalah dalam pengembangan lahan pasang surut dan lebak. Bahan Diskusi ' Coaching Petugas Pengelola tlsahatani Pertanian Pasang S u m dan Lebak". Dit. Perluasan Areal Pertanian, Ditjen Pertanian Tanaman Pangan; di Banjarbarn, Kalimantan Selatan, 2 - 7 September 1985. Kussow, W.R. 1971. Introduction to Soil Chemistry. Soil Fertility Project. IPB. 101 p.
Faperta,
Lashof, D.A. and D.R Ahuja. 1990. Relative contributionof greenhouse gas emission to global warming. Nature 344 : 529-531. Leiwakabessy, F.M. 1978. Siat lahan yang tersedia pada daemh transmigrasi. Seminar pemantapan usaha-usaha pembangunan di daerah transmigrasi oleh JKTI-PPSM.
Lindsay, W.L. 1979. Chemical equilibria in soils. John Wiley and Sans. New York.
A Willey-Interscience Publication.
Lucas, R.E. 1982. Organic soil (Histosol) formation, physical and chemical properties and management for crop production. Research Report 435 Farm Science. Maltby, E. 1997. Developing guidelines for the integrated management and sustainable utilisation of tropical lowlands peatlands. In: J. 0. Riley and S.E. Page (eds.). Biodiversity and sustainability aof tropical peat and peatlands. Proceeding of the International Symposium of biodiversity, environmental importance and sustainability of tropical peat and peatlands, Palangkaraya, Central Kalimantan 4 - 8 September 1999. Camara Publishing Ltd. Cardigan UK Mathur, S. P. and M. P. Lavesque. 1983. The effect of using copper for mitigating Histosol subsidence 01x2. The distribution of Cu, Mn, Zn and Fe in an organic soil, mineral sublayers and their mixtures in the context of setting a treshold of phytotoxic soil copper. 3. Soil Sci. 135(3): 166-176. Mario, M. D. dan I. G. M. Pandi. 2000. Pengaruh pemberian zeolit dan fosfat alam terhadap pertumbuhan dan produksi padi ditanah gambut. Jumal Ilmu Tanah dan Lingkungan Vol. 3 No. 1. IPB Press. 1-6. McKinzie, W.E. 1974. Criteria used in taxonomy to classification organic soils. In R.C. Dinauer (ed.) Histosols : Their Characteristics, Classification and Use. Soil %I. Amer. Madison. Mclaren, R. G. and D. V. Crawford. 1973. Studies on soil copper: I. The Fractionation of copper in soils. J. Soil Sci. 24(2):172-181. Miller, RW. and R.L. Donahue. 1990. Soil and Introduction to Soil and Plant Growth. Prentice Hall Englewood Clifts. New 3ersey. 768 p. Miyake, M. 1982. Improvement and management of peat soils in Japan. International sympozium and distributioan, characteristics and utilization of problem soils. Proc. Of a Symp. On Trop. Agr. Res, Series (15) 243-250. Morley, R. 3. 1981. Development and vegetation dynamics of lowland ombrogenous peat swamp in Kalimantan Tengah, Indonesia. 3. Biogeography 8: 383-404. Murali, V. and L. A. G. Aylmore. 1983. Competitive adsorption during solute transport in soils: 2. Simulations of competitive adsorption. Soil Sci. 135 (4):203-213. Neue, H.U., R.S. Lantin., Rainer Wassmann., J.B. Aduna., M.C.R. Alberto, and M.J.F. Andales. 1992. Methane emission from rice soils of the Philippines. pp. 55-63. Iff : K. Minami., A. Mosier, and R. Sass. CH4 and NzO, Global Emissions and Controls from Rice Fields and Other Agricultural and Industrial Sources. NIAES Series 2.
Orlov, D.S. 1995. Humic Substances of Soils and General Theory of Humification. Russian Translations Series 111. A.A. Balkerna Publ. USA. Ota, M., H. Kabayashi and M. Kawaguchi. 1957. The effect of slag on paddy soil. Soil and Plant Food. 1 : 45-46. Patrick, 2. A. 1971. Phytotoxic substance associated with the decomposition in soil of plant residues. Soil Sci. 111 : 13-18. Polak, 6. 1950. Occurrence and fertility of tropical peat soils in Indonesia. Inter. Congress of Soil Sci. 11: 183-185.
Proc.
Prasetyo, T. B. 1996. Prilaku asam-asam organik meracun pada tanah gambut yang diberi garam Na dan beberapa unsur mikro dalam kaitannya dengan hasil padi. Disertasi. Program Pascasarjana, Institut Pertanian Bogor. Bogor. Radjajagukguk, B. 1997. Peat soil of Indonesia. Locatioan, classification, and problems for sustainability. In: 3. 0. Riley and S.E. Page (eds.). pp 45 - 54. Biodiversity and sustainability a&f tropical pe& and p a t l a i d s proceeding of the ~ntemational Sym~osium of biodiversib, environmental im~ortance and sustainabilitv of tropkal peat and peatlands,. Palangkaraya, central Kalimantan 4 - 8 ~ e ~ t e m b e r 1999. Carnara Publishing Ltd. Cardigan UK. Rachim, A. 1995. Penggunaan kation-kation polivalen dalam kaitannya dengan ketersediaan fosfat untuk meningkatkan produksi jagung pada tanah gambut. Disertasi. Program Pascasarjana, Institut Pertanian -or. Riwandi. 2000. Kajian stabilitas gambut tropika Indonesia berdasarkan analisis kehilangan karbon organik, sifat fisiko kimia, dan komposisi bahan gambut. Disertasi. Program Pascasajana. Institut Pertanian Bogor. Sabiham, S. 1988. Studies on Peat in the coastal plain of Surnatera and Borneo. Part I: Physiography and geomorphology of the coastal plains. Tonan Ajia Kenkyu (Southeast Asian Studies). 26 (3): 307-335.
. 1996. Prospek pengelolaan lahan gambut untuk meningkatkan produksi beras nasionai. Makalah disampaikan pada Rapat Kerja Tahunan Rektor BKS PTN Wilayah Barat MIdi Universitas Palangkaraya, tanggal 7 Juni 19%.
.
1997. Penggunaan kation terpilih untuk menurunkan asam-asam fenolat toksik dalam Dnah gambut dari Jambi. 3. 11 Indon. Vol 7(1)1997.
. 2000. Kadar air kritis gambut Kalimantan Tengah datam kaitannya dengan kejadian kering tidak balik. Jumal Tanah Tropika Vol. V I No. 11. Fakultas Pertanian Univ. Lampung.
dan N. 8. E. Sulistyono. 2000. Kajian beberapa sifat inheren dan prilaku gambut: Kehilangan karbondioksida (C02) dan Metana (CH4) melalui proses reduksi-oksidasi. Jurnal Tropika Vol 5 (10). Fakultas Pertanian Univ. Lampung. dan Riwandi. 2000. Hubungan antara kandungan besi total dengan tingkat humifikasi dan derivat asam fenolat dalarn gambut Jambi dan Kalimantan Tengah. Jurnal Agrista Vol. 4 (1): 10-16. Fakultas Pertanian Univ. Syiah Kuala Darussalarn-Banda Aceh. Salarnpak. 1993. Studi asam fenol tanah gambut pedalaman dari Berengbengkel pada keadaan anerob. Tesis S2. Program Pascasarjana, Institut Pertanian Bogor. Bogor.
. 1999. Peningkatan produktivitas tanah gambut yang disawahkan dengan pernberian bahan amlioran tanah mineral berkadar besi tinggi. Disertasi. Program Pascasajana, Institut Pertanian Bogor. Saragih, E. S. 1996. Pengendalian asam-asarn organik meracun dengan penambahan Fe(II1)pada tanah gambut Jambi, Sumatera. Tesis S2. Program Pascasarjana, Institut Pertanian Bogor. Schnitzer, M. 1986. Binding o f humic substances by soil mineral colloids. Pp:77-102. In P. M. Huang and M. Schnitzer (Eds.). Interaction of Soil Minerals with Natural Organics and Microbes. SSSA Special Publication Number 17. Soil Soc. Am., Inc. Madison. and S.I.M. Skinner. 1967. Organo-metallic interaction in soils: 7. Stability constants of pb2+, Ni2+, co2+, Ca2+ and ~g"-fulvic acid complexes Soil Sci. 103 (4) : 247-252. Senesi, N. 1994. Spectroscopic studies of metal ion hurnic substance complexation in soil. In 15" World Congress of Soil Sci. Acapulco. Mexico. Shindo, H. and S. Kuwatsuka. 1975. Behavior of phenolic substances in the decaying process of plants. 111. Degradation pathway of phenolic acids. Soil Sci and Plant Nutr. 2 1 (3) : 227-238. Skoropanov, S. G. 1968. Redamation and Cultivation of Peat-Bog Soils. Israel Program for Scientific Translation Ltd., Jerusalem. Soil Survey Staff. 1975. Soil Taxonomy. USDA Agr. Hand Book 436. U.S. Government Printing Office. Washington D.C.
.
1998. Keys to Soil Taxonomy. Eight Edition. United State Department of Agriculture. Soil Conservation Service. USDA, Washington D.C.
. 1999. Soil Taxonomy : A Basic System of Soil Classification for Making and Interpreting Soiul Surveys. Soil Conservation Service. USDA, Washington D.C. Sollins, P., P. Homann, and B. A. Calldwell. 19%. Stabilzation and destabilization of soil organic matter: Mecanism and controls. Geoderma 74:65-105. Stevenson, F. J. 1994. Humus Chemistry. Genesis, composition, reactian. A WileyInterscience Pub!. John Wiley and sons. 2"d ed. New York-Chichester-BrisbaneToronto-Singapore. 496p.
. and A. Fitch. 1986. Reactions with organic matter. In J. F. Loneragan, A. D. Robson, and R. D. Graham (Eds.). Copper in Soil and Plants. Academic Press. Sydney. ., A. Fitch and M.S. Brar. 1993. Stability constant of Cu(n)-humate complexes. Comparison of select models. Soil Sci. 155 (2) : 77-91. Sulistyono, N.B.E. 2000. Peranan Kation Fe(1II) Terhadap produksi Karbon Dioksida dan Metana dari Gambut Tropika pada Inkubasi Aerob dab Anaerob. Tesis S2. Program Pascasajana IPB. Bogor. Suwamo and I.Goto, . 1997. Mineralogical and chemical properties of Indonesian electric furnace slag and its application effect as soil amandement. Setagaya. Tokyo. Agric. Sci. 3. 42 : 151-162. Tadsno, T., K. Yonebayashi, and N. Saito. 1992. Effect of phenolic acids on the growth and occurrence of sterility in crop plants. Pp: 358 - 369. In K. Kyuma, P. Vijarnsom, and A. Zakaria (eds.). Coastal lowland ecosystems in Southern Thailand and Malaysia. Showado-Printing Co., Skyoku. Kyoto. Takijima, Y. 1964a. Studies on organic acids in paddy field soils with reference to their inhibitory effects on the growth of rice plants. Part 1. Growth inhibiting action of organic acids and absorption and decomposition of them bay soils. Soil Sci. and Plant Nutr. lO(5): 14 - 21.
. 1964b. Studies on organic acids in paddy field soils with reference to their inhibitory effects on the growth of rice plants. Part 2. Relation between production of organic acids in waterlogged soils and the root growth inhibition. Soil Sc. And Plant Nutr. lO(5): 22 - 29. Tan, K. H. 1993. Principles of Soil Chemistry. Marcel Dekker, Inc. New York. 362p. Tim Inst'ltut Pertanian Bogor. 1974. Laporan survai produktivitas tanah dan pengembangan pertanian daerah Palangka Raya, Kalimantan Tengan. Bogor.
. 1976. Survai dan pemetaan tanah daerah Air Saleh, Sumatera Selatan. Proyek P4S, Ditjen Pangairan Dep. Pekerjaan Urnum dan Tenaga Listrik Institut Pertanian Bogor.
-
. 1986. Gambut pedalaman untuk lahan pertanian. Fakultas Pertanian, IPB bekerjasama dengan Dinas Pertanian tanaman Pangan Propinsi Dati IKalimantan Tengah. Bogor. Tisdale, S.L., W.L. Nelson and 3.0.Beaton. 1985. Soil Fertiliy and Fertilizers. 4a ed. The Macmillan Publ. Co.New York. 694 p. Tsusuki, K. 1984. Volatile products and low-molecular weight phenolic products of the anaerobic decomposition of organic matter, pp. 329-343. In Organic Matter and Rice. IRRI. Los banos Philippines. and R. Kondo. 1995. Lignis-derived phenolic compounds i n different types of peat profiles in Hokaido. Japan. Soil Sci. and Plant Nutr. 4 1 (3) : 515-527. Van Heuveln, B., A. Jongerius., and L. 3. Pons. 1960. Soil formation in organic soils. 7m Intern Congress of Soil Science, Madison. Wsc. USA. Wang, T.S.C.,
T.T. Yang dan T.T. Chang. inhibitors. Soil Sc. 103 : 239-246.
1967. Soil phenolic acids as plantgrowth
Widjaja-Adhi, I.P.G. 1988. Physical and chemical characteristics of peat mils of Indonesia. I A m J . 10(3) : 59-64.
.
1 7 . Pengelolaan lahan rawa dan gambut untuk usahatani dalam pengembangan berkelanjutan dan berwawasan lingkungan. Alami Vol. 2
(1) 28-35. Yagi, K. and Minami, K. 1990. Effect of organic matter application on methane emission from some 3apanese paddy fields. Soil Sci. Plant Nutr. 36:599-610.
LAMPIRAN
98
Tabel Larnpiran 1. Metoda Analisis Sifat Kimia Tanah
Sifat Kimia Tanah
Metoda Analisis
pH Hz0 (1:5)
Elektroda gelas (Black, 1965)
N-total
Kjeldahl (Bremner, 1996)
P-tersedia
Bray
Basa-basa tersedia
1 N NH40ac pH 7,O (Black, 1965)
I (Black, 1965)
C-organik Tanah gambut
1987) Gravimetri (Blakemore eta/.,
Tanah mineral
Walkley dan Black (Black, 1965)
Unsur rnikro larut
0,05 NHCI (Ambak, eta/., 1991)
Unsur mikro total
HC104-HN03 pekat (Page et dl., 1982)
Kadar abu
Gravimetri (Blakemare eta/., 1987)
KTK
1 NNH40ac pH 7,O (Black, 1965)
KB
F . Basa-basa / KTK
Tabel Lampiran 2. Diskripsi Profil Tanah Garnbut Berengbengkel (Pedalarnan), Sampit (Transisi), dan Garnbut Samuda (Pantai) Kalirnantan Tengah.
Lokasi (I) Klasifikasi Tanah Penggunaan lahan Vegetasi Diskripsi profil Simbol Horison Oa Oe Oe Oi
: Berengbengkel (Garnbut Pedalarnan) : Tipik Haptohemist, disik, isohipetermik : Tegalan, semak Kedalaman bahan organik : 510 crn : Paku-pakuan Kedalaman air tanah : 35 cm
Kedalarnan (cm) 0 50 125 275
-
Lokasi (11) Klasfikasi tanah Penggunaan lahan Vegetasi
50 125 275 510
Warna Munsel
Dekornposisi/ Tekstur
Kadar serat (%)
10YR4/4 10YR6/4 10YR7/3 1OYR5/8
Saprik Hemik Hernik Fibrik
15 30 35 60
C-Org
(%I
pH Hz0
56.4 57.7 57.7 57.8
3.7 3.7 3.8 3.8
: Sarnpit (Garnbut Transisi) : Tipik Haplohemist, disik, isohipetermik : semak Kedalarnan bahan organik : 220 cm : Paku-pakuan Kedalarnan air tanah : 30 crn
Diskripsi profil
Simbol Horison Oe Oe Oi
Kedalaman (cm) 0 - 50 50 - 150 150 - 220
Warna Munsel 10YR4/4 10YR6/4 10YR6/6
Dekomposisi/ Tekstur
Kadar serat (%)
Hemik Hernik Fibrik
25 30 40
C-Ora (%f 57.8 57.8 57.8
pH Hz0 3.8 3.6 3.7
Lokasi (111) : Handil Sohor, Sarnuda (Garnbut Pantai) : Tipik Sulfihemist, isohipetermik Kfasifikasi Tanah Penggunaan lahan : semak Kedalarnan bahan organik : 115 cm Vegetasi : Paku-pakuan Kedalaman air tanah : 30 crn Diskripsi profil Simbol Kedalaman Wama Dekornposisi/ Kadar C-Org pH PH Horison (cm> Munsel Tekstur setat (9-6) (5%) H20 H,02 Oa Oe Oi C
0 25 70 115
-
-
25 70 115 160
10YR4/4 10YR5/8 10~~5/8 10YR5/8
Hemik Hernik Fibrik Liat berpasir
19 39 56
54.4 56.4 56.4
4.0 4.1 4.1 4.5
2.35 2.40 2.35 2.00
Tabel Lampiran 3. Kriteria Penilaian Kandungan Unsur dan kernasaman Tanah Daerah Pasan Surut.
Ciri Tanah Rendah
Tinqkat Sedang
Tingqi
-
N-total (%)
< 0,2
0,2
0,5
> 0,s
P-Bray I (pprn)
< 7,O
7,O - 30,O
> 30,O
K-dd (rne/100 g )
< 0,83
0,83 - 3/25
> 3/25
Cu ekstraksi 0,05 NHCl (pprn)
-= 9,O
9,O - 20,O
> 20,O
Zn ekstraksi 0,051NHCl (ppm)
< 2,5
2,s - 10,O
> 10,O
Mn ekstraksi 0,05 NHCI (ppm)
5,6
Masarn ekstrim
Sumber :Rachim (1995)
- 6,O
Masam sedang
6,l - 6,5 masarn
6,6
- 7,3
Netral
Tabel lampiran 4. Komposisi Kimia Bahan Amelioran Terak baja (Electric Furnace Slag) *) No
Komposisi Kimia Contoh 1
Nomor Contoh Contoh 2 Contoh 3
) Dianalisis Berdasarkan Metoda Lithium Metaborate Fusion
4. MgO
Rata-rata
I
(g.kg-')
5 . A1203 ( 9 . k ~ - I )
6 . P205 (g.kg-l)
7 . Mn02 (g.kg-I) 8. K20
@.kg-')
9. N a 2 0 (g.kg")
2.1
2.2
1.2
1,8
3,9
3,5
2.4
3.3
65,7
66,3
619
849
Dianalisis Berdasarkan Metoda Acid digestion
13.8
(mg.kg-I)
51.3
81.8
14. Cr
(mg.kg-')
1267
661
*) Sumber : Suwamo (1998)
Tabel Lampiran 5.
Sifat Kimia Tanah Bahan Arnelioran Tanah Mineral dari Pundu-Kasongan Kalimantan tengah.
Sifat Kimia Tanah
I
Metoda Analisis
1 Elektroda gelas C-organik (%)
Walkley dan Black
N-total (%)
Kjeldahl
P-tersedia (ppm)
Bray I
-
Basa-basa (me1100 g)
Ca Mg K Na Total KTK (me/100 g) 7.
Kejenuhan basa (%)
8.
Af (me1100 g)
9.
Unsur Mikro (ppm) EDTA EDTA EDTA EDTA Metal oksida Fe203 A1203
Puslitbang Tek. Mineral Pusfitbang Tek. Mineral
Basa oksida (%) CaO MgO K20
HCI 25% HCI 25% HCI 25%
Tekstur (%) Pasir Debu Liat
Pipet Pipet Pipet
I
I Sumber : Salarnpak (7999).
Tabel Lampiran 6. Kelarutan Fe dari Tanah Mineral yang Diperkaya oleh Bahan Berkadar Besi tinggi (pglg)
Tabel Lampiran 7.Hasit Analisis Beberapa Derivat Asam Fenolat dalam Tanah gambut Berengbengkel (pedalaman), Sarnpit (Traansisi), dan Samuda (Gambut Pasang Surut) yang Diberi Perlakuan Bahan Amelioran Perlakuan
Ulangan
Gambur Pedalaman (Berengbengkel)
Gambut Transisi (Sampit)
Gambut Pasang Surut (Samuda)
0.9669 0.8514 0.9092 0 6743 0.6533 0.6638 0.6836 0.6608 0.6722 0.6924 0.6821 0.6873 0.7022 0.6795 0.6909 0.7196 0.69 17 0.7057 0.7257 0.7150 0 7204 0.7305 0.7098 0.7202
0.7982 0.8011 0.7997 0.591 7 0.5734 0.5826 0.5899 0.6070 0.5985 0.6116 0.5963 0.6040 0.6023 0.6254 0.6139 0.6440 0.6149 0.6295 0.6367 0.6693 0.6530 0.6584 0.6756 0.6670
0.6873 0.6609 0.6471 0.4883 0.4902 0.4893 0.4895 0.5 100 0.4998 0.5067 0.4988 0.5028 0.4931 0.5116 0.5024 0.5155 0.51 19 0.5137 0.5049 0 5127 0.5088 0.5140 0.525I 0.5196
Asam Hidroksibenzoat (mM)
A0
1 2
I
A1
2
A2
1 2
A3
2
A4
I 2
A5
2
A6
2
A7
1 2
Asarn Vanilat (mM)
I
I I
Tabel Larnpiran 7 (Lanjutan)
Perlakuan
Ulangan
Gambut Pedalaman (Berengbengkel)
Gambut Transisi (Sampit)
Gambut Pasang Sumt (Samuda)
Tabel Lampiran 7 (lanjutan) Perlakuan Ulangan Gambut Pedalarnan (Berengbengkel)
Gambut Transisi (Sarnpit)
Garnbut Pasang Sumt (Sarnuda)
Asam Ferulat (mM)
1
Asarn Sinapat (mM)
I
Tabel Lampiran 8. lnteraksi Asam-asam Fenolat (%) Dari Tanah Gambut Berengbengkel, Sarnpit dan Samuda dengan Tanah Mineral yang Diperkayan Oleh Bahan Berkadar Besi Tinggi Perlakuan
ULangan
Gambut Pedalaman (Berengbengkel)
Gambut Transisi (Sampit)
Gambut Pantai (Samuda)
28.29 23.27 25.78 29.30 22.39 25.84 28.39 19.88 24.14 27.38 20.19 23.79 25.58 18.76 22.17 24.95 16.02 20.49 24.45 16.63 20.54
25.87 28.42 27.15 26.10 24.23 25.17 23.38 25.57 24.48 24.54 21.93 23.24 19.32 23.24 21.28 20.23 16.45 18.34 17.51 15.67 16.59
28.95 25.83 27.39 28.78 22.83 25.81 26.28 24.53 25.40 28.26 22.59 25.42 25.00 22.55 23.78 26.54 22.42 24.48 25.22 20.55 22.88
Hidroxybenzoic acid (%) A1
1 2
x
A2
1 2
-x A3
1 2
x A4
1 2
x A5
1 2 X
A6 A7
1 2 X 1 2
x Vanilic acid (%)
Tabel Larnpiran 8 (Lanjutan)
Perlakuan
Ulangan
Syringic acid (%)
p-Coumaric acid (%)
Gambut Pedalaman (Berengbengkel)
Gambut Transisi (Sampit)
Gambut Pantai (Samuda)
Tabel Larnpiran 8 (Lanjutan)
Perlakuan
Ulangan
Gambut Pedalaman (Berengbengkel)
Garnbut Transisi (Sarnpit)
Garnbut Pantai (Sarnuda)
31.44 33.73 32.58 30.55 27.72 29.13 29.22 26.68 27.95 27.39 23.74 25.56 26.92 20.74 23.83 27.06 21.15 24.1 1 19.33 19.23 19.28
48.27 38.17 43.22 47.64 37.26 42.45 44.65 34.17 39.41 35.71 30.23 32.97 30.94 24.42 27.68 28.84 23.74 26.29 27.84 23.38 25.61
44.52 48.27 46.39 44.20 46.69 45.44 40.90 44.27 42.58 37.43 42.80 40.1 1 33.96 40.61 37.28 30.31 40.02 35.16 24.36 35.03 29.70
( Ferulic acid (%) A1
1 2 -
x
A2
1 2 -
x
A3
1 2 -
x
A4
1 2 x
A5
1
2 -
x
A6
1 2 -
A7
x 1
2 x
Sinapic acid
(Oh)
I
i
abel Lampiran 9.
Pengaruh Pemberian Tanah mineral yang Diperkaya oleh Bahan Berkadar Besi Tinggi Terhadap Sifat Kimia Tanah Gambut Berengbengkel (pedalaman), Gambut Sampit (transisi), dan Gambut Samuda (Pantai),
Tabel Lampiran 9 (Lanjutan)
Gambut Samuda (Pantai)
Tabel Larnpiran 9 (Lanjutan) Garnbut Sampit (Transisi)
Tabel Lampiran 10. Pengaruh Pemberian Tanah Mineral yang Diperkaya Oleh Bahan Berkadar Besi Tinggi Terhadap Emisi CH4dan C02 pada Tanah Gambut Pedalaman Berengbengkel, Gambut Transisi Sampit dan Gambut Pantai Samuda.
Tabel Lampiran 11. Data Rata-rata Temperatur Sungkup OC (T,), Perubahan Konsentrasi Metan dalam Sungkup setelah Periode t Menit (G[CH,]/St), Laju Emisi Metan mg.m-2jam-1(bM), dan Standar Deviasi (Stdev) pada Gambut Pantai Samuda, Gambut Pedalaman (Berengbengkel) dan Gambut Transisi (Sampit). Garnbut Pantai (Samudal 0 MST
Perlakuan
Tu
G[CH4]/St $M
4 MST
8 MST
Stdev
T,
6[CH4]/6t
4M
Stdev
T, 6[CH4]/St 4M Stdev
A0
40.3
0.1631
6.14
0.23
41.5
0.1841
6.90
0.57
40.5
0.2198
8.27
A1
41.5
0.1113
4.17
0.39
42.0
0.1351
5.06
0,11
41.0
0.1630
6.12 0.10
A2
42.0
0.1207
4.52
0.31
41.0
0.1321
4.96
0.21
42.5
0.1459
5.45
0.78
A3
41.5
0.1288
4.83
0.67
41.5
0.1360
5.10
1.26
39.7
0.1389
5.24
0.24
A4
40.6
0.1322
4.97
0.12
43.0
0.1488
5.55
0.63
41.0
0.1489
5.59
0.23
0.35
(Tabel lampiran 11(Lanjutan) Garnbut Pedalarnan (Berenclbenqkel) -
0 MST Perlakuan
4 MST
8 MST
Tu 6[CH4]/6t gM Stdev
G[CH4]/St gM
Stdev
42.0
0.1972
7.38
0.51 40.5 0.1871 7.04 0.12
0.1369 5.11 0.14
40.5
0.1619
6.09
0.52 41.0 0.1401 5.26 0.20
41.5
0.1198 4.49
0.11
43.0
0.1587 5.92
0.54 42.0 0.1696 6.35 1.12
A3
40.0
0.1362 5.13
0.27
42.6
0.1561 5.83
0.22 42.0 0.1824 6.83 0.15
A4
42.6
0.1297 4.85
0.14
41.9
0.1614 6.04
0.17 41.4 0.1765 6.62 1.16
A5
43.1
0.1412 5.27
0.09
41.5
0.1604 6.01
1.22 41.4 0.1733 6.50 0.72
A6
41.0
0.1313 4.93 0.78
43.0
0.1776 6.63
0.02 42.0 0.1813 6.79 0.43
A7
44.0
0.1547 5.75 0.02
42.8
0.1700 6.35
0.11 41.5 0.1863 6.98 0.15
T,
6[CH4]/6t gM
Stdev
T,
A0
43.5
0.1712 6.38
0.32
A1
42.8
A2
Tabel Larnpiran 11 (Lanjutan).
Gambut Transisi (Sam~it)
Tabel Lampiran 12. Data Rata-rata Temperatur Sungkup "C (T,), Perubahan Konsentrasi COz dalam Sungkup setelah Periode t Menit (G[CH4]/Ft), Laju Emisi COz rng.m'2jam'1 (gM), dan Standar Deviasi (Stdev) pada Gambut Pantai Samuda, Gambut Pedalaman (Berengbengkel) dan Gambut Transisi (Sampit). Gambut Pantai (Samuda] 0 MST
Perlakuan
Tu
A0
4 MST
8 MST
Stdev
Tu
6[CH4]/6t
gM
Stdev
40.3
0.5571 57.21 3.57
41.5
0.5913
60.49
4.63
40.5
0.7499 76.96 3.00
A1
41.5
0.3879 39.68
2.64
42.0
0.3713
37.92
3,19
41.0
0.4704 48.20 5.67
A2
42.0
0.4062 41.49
LO7
41.0
0.4157
42.59
8.16
42.5
0.4886 49.82 5.67
A3
41.5
0.4396 44.97
9.79
41.5
0.4229
43.27
1.75
39.7
0,4722 48.59 7.17
A4
40.6
0.4228 43.37
9.58
43.0
0.4780
48.66
1.95
41.0
0.4886 50.06 10.39
s[CH,]/Gt
gM
Tu 6[CH4]/6t
$M Stdev
(Tabel larnpiran 12 (Lanjutan) Gambut Pedalaman (Berenobenqkel)
0 MST
4 MST
8 MST
Tabel Lampiran 12 (Lanjutan).
Gambut Transisi (Sarnoit]
I
0 MST
4 MST
I
Tabel Lampiran 13. Rata-rata Pengamatan Tinggi Tanaman, Anakan Maksimum, dan Anakan Produktif Akibat Pemberian Amelioran pada Tanah Gambut Berengbengkel (Pedalaman), Gambut Sampit (Transisi) dan Garnbut Sarnuda (Pantai).
Keterangan : Angka-angka yang diikuti oleh huruf yang sama tidak berbeda nyata berdasarkan Uji Tukey pada taraf a = 5%