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Mineralogical Characteristics and The Pedogenetic Processes of Soils on Coral Reefs in Ambon Rina Devnita
Indonesian Journal on Geoscience Vol 4, No 1 (2009)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (450.848 KB) | DOI: 10.17014/ijog.4.1.19-29

Abstract

http://dx.doi.org/10.17014/ijog.vol4no1.20093The mineralogical characteristics of soils developed on coral reef parent materials in Hitu and Wailiha, Ambon, were investigated regarding to the relationship to pedogenesis. The analyses concerned with the characteristics of soil chemical, physical, and mineralogy of the rock fragment and sand, silt and clay fractions are to investigate the pedogenesis processes. Both soil profiles indicate the clayey texture, slightly neutral reaction, high cation exchange capacity, base saturation, and iron oxide. The mineralogical analyses of rock fragments and sand fractions indicate that besides carbonate minerals, silicate minerals were also found. The clay mineralogy showing the domination of kaolinite, gibbsite, and goethite, reflects that the soil is intensely weathered. Pedogenesis process showing the clay translocation, indicates that the weathering process has been occuring under the tropical influence.    
Melanic and Fulvic Andisols in Volcanic Soils derived from some Volcanoes in West Java Rina Devnita
Indonesian Journal on Geoscience Vol 7, No 4 (2012)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1545.538 KB) | DOI: 10.17014/ijog.7.4.227-240

Abstract

DOI: 10.17014/ijog.v7i4.149Melanic and fulvic Andisols are the great groups in the classification of volcanic soils Andisols, which describe the soils with high organic carbon content in the epipedon. The organic C must be more than 6% in the upper 30 cm with the value and chroma are 2 or less for melanic and more than 2 for fulvic. Melanic epipedon also has to have the melanic index that is 1.70 or less. The objective of this study is to investigate the melanic and fulvic Andisols in volcanic soils that developed under pine forest vegetation (Pinus merkusii) from different parent materials and ages of Mount Tangkuban Parahu (andesitic, Holocene) and Mount Tilu (basaltic, Pleistocene). The method used was a descriptive comparative survey of three profiles in Mount Tangkuban Parahu and three profiles in Mount Tilu. Analyses were done for each horizon in the profiles comprising the investigation of andic soil properties through the analyses of organic C, bulk density, Al + ½ Fe (ammonium oxalate), and P-retention. The investigations were continued by further calculation of organic C content and by investigation of soil colour with Munsell Soil Colour Chart. The results showed that the two profiles in Mount Tangkuban Parahu and two profiles in Mount Tilu are fulvic Andisol. No melanic Andisols were found in both locations. Pine forest vegetation encourages the formation of fulvic Andisols were derived from andesitic-Holocene parent materials or basaltic-Pleistocene parent materials.
The Investigation of Ultic Horizon on Andisols Derived from the Eruption of Mount Tilu (Pleistocene, Basaltic) in West Java, Indonesia Rina Devnita; Emi Sukiyah; Apong Sandrawati
Indonesian Journal on Geoscience Vol 9, No 2 (2022)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17014/ijog.9.2.159-172

Abstract

DOI:10.17014/ijog.9.2.159-172Ultic is the soil characteristics in soil taxonomy when argillic or kandic horizon is found within the depth of 125 cm with the base saturation of less than 35 % on the overall of upper 50 cm. The purpose of this research is to investigate whether ultic horizon was found in the soil developing from the Pleistocene eruption of Mount Tilu (basaltic parent materials), in West Java, Indonesia. The method used was descriptive and comparative surveys of three profiles in the area around Mount Tilu, including the investigation of andic soil properties and the formation of argillic or kandic horizon. The result showed that the soils fulfilled the requirements of andic soil properties to be classified as Andisols. Soil never dried for ninety days cumulative (udic) to be classified as Udands. There were Fulvudands and Hapludands in this location. Accumulation of clays was more than 1.2% higher than the overlying horizon found at the depth of 90, 79, and 51 cm in those three profiles. Base saturation in upper 50 cm ranged from 1.07 to 6.86 cmol kg-1 or less than 35 %, making the soils were classified as Ultic Fulvudands and Ultic Hapludands. The high rainfall in the tropics and Pleistocene age led to the leaching of clays for a long period to form the argillic horizon. The influence of rain was stronger than the basaltic parent materials in forming Ultic Hapludands. Basaltic parent material was not strong enough to produce base saturation of more than 35 %.
Pengaruh Terak Baja dan Bokashi Sekam Padi terhadap Kemantapan Agregat dan BiomassaTanaman Jagung pada Andisol, Lembang Henly Yulina; Rina Devnita; Rachmat Harryanto
Agro Wiralodra Vol. 1 No. 1 (2018): Jurnal Agro Wiralodra
Publisher : Universitas Wiralodra

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31943/agrowiralodra.v1i1.7

Abstract

Andisol mempunyai sifat fisika tanah yang baik, namun bermasalah dengan retensi P. Pemberian amelioran untuk mengurangi retensi P, diharapkan dapat mempertahankan bahkan meningkatkan parameter fisika tanah tersebut. Penelitian bertujuan untuk mengetahui interaksi terak baja dengan bokashi sekam padi terhadap kemantapan agregat dan biomassa tanaman jagung manis pada Andisol Lembang. Penelitian menggunakan Rancangan Acak Kelompok Pola Faktorial dengan dua faktor. Faktor pertama terak baja dan faktor kedua bokashi sekam padi masing- masing 4 taraf : 0%, 2,5%, 5,0%, dan 7,5%, diulang dua kali. Hasil penelitian menunjukkan bahwa terdapat interaksi antara terak baja dengan bokashi sekam padi terhadap kemantapan agregat tanah pada jagung manis setelah panen dan biomassa tanaman jagung manis. Kombinasi dosis 5,0% terak baja dan 7,5% bokashi sekam padi memberikan hasil terbaik terhadap kemantapan agregat tanah pada jagung manis setelah panen dan biomassa tanaman jagung manis, kombinasi 2,5% terak baja dan 7,5% bokashi sekam padi memberikan hasil terbaik.
Hubungan Bobot Isi dan Kemantapan Agregat Tanah Andisol Lembang terhadap Biomassa Tanaman Jagung Manis setelah dilakukan Kombinasi Terak Baja dan Bokashi Sekam Padi Henly Yulina; Rina Devnita; Rachmat Harryanto
Agro Wiralodra Vol. 1 No. 2 (2018): Jurnal Agro Wiralodra
Publisher : Universitas Wiralodra

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31943/agrowiralodra.v1i2.11

Abstract

Penelitian ini bertujuan untuk mengetahui hubungan bobot isi dan kemantapan agregat tanah Andisol Lembang terhadap biomassa tanaman jagung manis. Penelitian menggunakan Rancangan Acak Kelompok Pola Faktorial dengan dua faktor. Faktor pertama terak baja dan faktor kedua bokashi sekam padi masing-masing 4 taraf, yaitu 0%, 2,5%, 5,0% dan 7,5%, diulang dua kali. Hubungan antara masing-masing perlakuan selanjutnya di analisis menggunakan model regresi linier sederhana. Hasil penelitian menunjukkan bahwa terdapat hubungan antara bobot isi, kemantapan agregat tanah dengan biomassa tanaman jagung manis, namun biomassa tanaman jagung manis tidak dipengaruhi oleh bobot isi dan kemantapan agregat.
Hubungan Porositas Tanah Dan Air Tersedia Dengan Biomassa Tanaman Jagung Manis Dan Brokoli Setelah Diberikan Kombinasi Terak Baja Dan Bokashi Sekam Padi Pada Andisol, Lembang Henly Yulina; Rina Devnita; Rachmat Harryanto
Agro Wiralodra Vol. 2 No. 2 (2019): Jurnal Agro Wiralodra
Publisher : Universitas Wiralodra

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31943/agrowiralodra.v2i2.16

Abstract

Penelitian bertujuan untuk mengetahui hubungan antara porositas tanah dan air tersedia terhadap biomassa tanaman jagnung manis dan brokoli setelah diberikan kombinasi terak baja dan bokashi sekam padi pada Andisol Lembang. Penelitian menggunakan Rancangan Acak Kelompok Pola Faktorial dengan dua faktor. Faktor pertama terak baja dan faktor kedua bokashi sekam padi masing- masing 4 taraf : 0%, 2,5%, 5,0%, dan 7,5%, diulang dua kali. Hasil penelitian menunjukkan bahwa terdapat hubungan antara porositas tanah dan air tersedia dengan biomassa tanaman jagung manis dan brokoli, namun biomassa kedua tanaman tidak dipengaruhi oleh porositas tanah dan air tersedia tersebut namun dipengaruhi oleh faktor fisika tanah lain, seperti bobot isi dan kemantapan agregat tanah.
RESPON BOBOT ISI, KEMANTAPAN AGREGAT, DAN POROSITAS TANAH PADA TANAMAN CABAI MERAH SETELAH VEGETATIF AKHIR TERHADAP KOMBINASI TERAK BAJA DAN BOKASHI SEKAM PADI PADA ANDISOL, LEMBANG Henly Yulina; Rina Devnita; Rachmat Harryanto
Agro Wiralodra Vol. 2 No. 1 (2019): Jurnal Agro Wiralodra
Publisher : Universitas Wiralodra

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31943/agrowiralodra.v2i1.26

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Penelitian ini bertujuan untuk mengetahui respon bobot isi, porositas, dan kemantapan agregat tanah pada tanaman cabai merah setelah vegetatif akhir terhadap kombinasi terak baja dengan bokashi sekam padi pada Andisol Lembang. Penelitian menggunakan Rancangan Acak Kelompok Pola Faktorial dengan dua faktor. Faktor pertama terak baja dan faktor kedua bokashi sekam padi masing- masing 4 taraf : 0%, 2,5%, 5,0%, dan 7,5%, diulang dua kali. Hasil penelitian menunjukkan bahwa tidak terjadi interaksi antara terak baja dengan bokashi sekam padi terhadap bobot isi dan porositas tanah, namun terak baja dan bokashi sekam padi berpengaruh mandiri terhadap kemantapan agregat tanah pada tanaman cabai merah setelah vegetatif akhir. Penurunan bobot isi dan peningkatan porositas tanah terbesar terjadi pada dosis 7,5% (b3), sedangkan penurunan kemantapan agregat tanah terbesar terjadi pada dosis 5,0% (t2) terak baja (4,38) dan dosis 7,5% (b3) bokashi sekam padi (3,25), namun dengan pemberian masing- masing dosis 2,5% pada terak baja (t1) dan bokashi sekam padi (b1) sudah dapat menurunkan nilai kemantapan agregat tanah
Respons Aplikasi Partikel Nano Abu Vulkanik dan Batuan Fosfat terhadap Beberapa Sifat Kimia Tanah Inceptisols Cilembu, Jawa Barat Pradhinto Dwi Nugroho; Mahfud Arifin; Rina Devnita
Jurnal Tanah dan Iklim (Indonesian Soil and Climate Journal) Vol 44, No 2 (2020)
Publisher : Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21082/jti.v44n2.2020.109-116

Abstract

Abstrak. Kandungan dan ketersediaan unsur P,  yang merupakan unsur esensial,  rendah pada Inceptisols Cilembu. Unsur P dalam bentuk partikel nano diharapkan dapat mudah diserap oleh tanah. Penelitian ini bertujuan mengetahui pengaruh amelioran partikel nano (abu vulkanik dan batuan fosfat) terhadap P-tersedia dan kemasaman tanah (pH-H2O), serta kapasitas tukar kation (KTK) tanah Inceptisols Cilembu, Sumedang, Jawa Barat. Penelitian dilaksanakan pada bulan Januari sampai dengan Juni 2019 di Laboratorium Fisika Tanah Departemen Ilmu Tanah dan Sumber Daya Lahan, Fakultas Pertanian, Universitas Padjadjaran. Metode penelitian menggunakan Rancangan Acak Lengkap Faktorial. Penelitian dilakukan dengan inkubasi partikel nano abu vulkanik dan batuan fosfat dengan dosis masing-masing 0% (0 g), 2% (20 g per kg tanah), 4% (40 g per kg tanah) dan 6% (60 g per kg tanah). Hasil penelitian menunjukkan tidak terjadi interaksi antara partikel nano abu vulkanik dan batuan fosfat terhadap P-tersedia dan kemasaman tanah (pH-H2O) dan kapasitas tukar kation (KTK). Partikel nano abu vulkanik dan batuan fosfat terlihat nyata berpengaruh terhadap P tersedia setelah inkubasi bulan pertama dan bulan kedua. Penggunaan partikel nano abu vulkanik berpengaruh nyata terhadap meningkatnya pH setelah inkubasi bulan pertama. Interaksi partikel nano abu vulkanik dan partikel nano batuan fosfat tidak berpengaruh nyata terhadap nilai KTK.Abstract. The content and availability of P, which is an essential element in Cilembu Inceptisols. is low. P element in the form of nano particles is expected to increase P availability. The aim of the study was to evaluate the effect of Ameliorant nanoparticles (volcanic ash and phosphate rock) on P availability and soil acidity (pH-H2O) as well as cation exchange capacity (CEC) in Inceptisols Cilembu, Sumedang, West Java. This research conducted in January to June 2019 in the Soil Physics Laboratory of the Department of Land Science and Land Resources, Faculty of Agriculture, Padjadjaran University. The research used Factorial Completely Randomized Design. The study carried out by incubation of volcanic ash nano particles and phosphate rocks with doses of 0% (0 g), 2% (20 g per kilograms of soil), 4% (40 g per kilograms of soil) and 6% (60 g per kilograms of soil). The results showed no interaction between volcanic ash nano particles and phosphate rocks on available P, soil acidity (pH-H2O) and cation exchange capacity (CEC). The effect of nano particles of volcanic ash and phosphate rock was significantly affected by available P after incubation of the first and second months. The use of nano volcanic ash particles has a significant effect on increasing pH after the incubation of the first month. Interaction effect of volcanic ash nano particles and phosphate rock nano particles was not significant on CEC value.
Pengaruh Amelioran Partikel Nano Batuan Fosfat dan Jamur Pelarut Fosfat terhadap Sifat Kimia Inceptisols Cilembu, Jawa Barat Fajri Syahid Nurhakim; Pujawati Suryatmana; Muhammad Amir Solihin; Rina Devnita; Mahfud Arifin
Jurnal Tanah dan Iklim (Indonesian Soil and Climate Journal) Vol 44, No 2 (2020)
Publisher : Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21082/jti.v44n2.2020.155-162

Abstract

Abstrak. Inceptisols Cilembu memiliki potensi besar untuk pertanian khususnya untuk budidaya ubi jalar Cilembu. Rendahnya kandungan P-tersedia yang merupakan unsur hara esensial berdampak pada produktivitas tanah. Aplikasi amelioran partikel nano batuan fosfat dan Jamur Pelarut Fosfat (JPF) memiliki kemampuan dalam meningkatkan P-tersedia Inceptisols Cilembu. Penelitian ini bertujuan untuk mengkaji pengaruh amelioran partikel nano batuan fosfat dan JPF terhadap beberapa sifat kimia Inceptisols di sekitar Cilembu. Metode penelitian menggunakan Rancangan Acak Lengkap Faktorial. Faktor pertama yaitu amelioran partikel nano batuan fosfat yang terdiri atas empat taraf, yaitu b0 = 0% (0 g), b1 = 2% (20 g kg-1 tanah), b2 = 4% (40 g kg-1  tanah), dan b3 = 6% (60 g kg-1 tanah). Faktor kedua yaitu JPF yang terdiri atas dua taraf, yaitu h0 = (0 g) dan h1 = JPF (10 g per kg-1 tanah). Parameter yang diamati: pH, P-tersedia, Kapasitas Tukar Kation (KTK), dan populasi JPF. Data hasil pengamatan dianalisis menggunakan analisis varians pada taraf 5%, dilanjutkan dengan uji beda jarak Duncan pada taraf 5%. Hasil analisis varians menunjukkan tidak terdapat interaksi antara amelioran partikel nano batuan fosfat dan JPF terhadap parameter yang diamati. Aplikasi amelioran partikel nano batuan fosfat berpengaruh nyata dalam meningkatkan pH dan P-tersedia. Penggunaan JPF berpengaruh nyata meningkatkan nilai KTK.Abstract. Inceptisols in Cilembu have a great potential for agriculture, especially for sweet potato cultivation. The low available P content, which is an essential nutrient, has an impact on soil productivity. The application of nano particle phosphate rock ameliorant and Phosphate Solubilizing Fungi (PSF) may increasing available P of Inceptisols in Cilembu. The research aimed to find out the effects of nano particle phosphate rock ameliorant and PSF on selected chemical properties of Inceptisols in Cilembu area. The research method used Factorial Completely Randomized Design. The first factor was ameliorant nano particles of phosphate rock application consisted of four levels, namely b0 = 0% (0 g), b1 = 2% (20 g kg-1 of soil), b2 = 4% (40 g kg-1 of soil), b3 = 6 % (60 g kg-1 of soil). The second factor was PSF treatment consisted of two levels, namely h0 = without PSF and h1 = PSF 10 g kg-1 of soil. Parameters observed were pH, available P, Cation Exchange Capacity (CEC), and PSF population. The data were analyzed with analysis of variance at the significance level of 5%, and continued with Duncan multiple range test at the significance level of 5%. The results showed that there was no interaction between ameliorant nano particles of phosphate rock application and PSF inoculation on the observed parameters. The application of ameliorant nano particles of phosphate rock significantly increased soil acidity (pH) and available P. The inoculation of PSF significantly increased the CEC.
Pengaruh Terak Baja Dan Bokashi Sekam Padi Terhadap Sifat Fisika Tanah Pada Andisol Rina Devnita; R Hudaya; F Rosana
Agrologia Vol 3, No 1 (2014): Agrologia: Jurnal Ilmu Budidaya Tanaman
Publisher : Faculty of Agriculture, Pattimura University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30598/a.v3i1.254

Abstract

Andisols are considered as productive soils, but their P-retention have to be reduced to increase the available P.  This research concerning the remediation of Andisols with steel slag and bokashi of husk to overcome the P problem and to investigate their  influence  to soil physical aspects.  The treatments were arranged in Randomized Block Designed in factorial pattern with two factors: steel slag and bokashi of husk, consisted of four level: 0, 2.5, 5.0 and 7.5 % of soil weight (w/w). The treatments were repeated twice, brought a combination of 4 x 4 x 2.  The soils with each treatments were mixed thoroughly, filled into the polybags, watered to the field capacity, closed tightly, incubated for four months, and sampled for chemical and physical analyses. The parameters were P-retention, bulk density, permeability and aggregate stability.  The result showed that steel slag and bokashi of  husk were interacted in decreasing P-retention.  These combination had no effect to soil physical characteristics which mean that the treatments did not aggravate the bulk density, soil permeability and aggregate stability. The remediation of Andisol with steel slag and bokashi of husk decreased the P-retention, and kept the good aspects of soil physical characteristics.