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All Journal Journal of Tropical Soils JTSL (Jurnal Tanah dan Sumberdaya Lahan) Journal of Degraded and Mining Lands Management Jurnal Pembangunan dan Alam Lestari agriTECH Jurnal Teknik Pertanian Lampung (Journal of Agricultural Engineering) Jurnal Penelitian Kehutanan Bonita Jurnal Riset Kajian Teknologi dan Lingkungan
Sugeng Prijono
Universitas Brawijaya
Agriculture, Biological Sciences & Forestry Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Decision Sciences, Operations Research & Management Economics, Econometrics & Finance Engineering Environmental Science Languange, Linguistic, Communication & Media Materials Science & Nanotechnology Social Sciences Other

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Effect of Coffee Ages and Shade Types on Soil Moisture and Soil N, P, K Availability in UB Forest sa'diyah, zenny faridatus; Prijono, Sugeng; Suntari, Retno; Kusuma, Zaenal
JOURNAL OF TROPICAL SOILS Vol. 28 No. 2: May 2023
Publisher : UNIVERSITY OF LAMPUNG

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.5400/jts.2023.v28i2.39-45

Abstract

Water and nutrients is important for plant which has its characteristics. This study has been carried out in the UB (Brawijaya University) forest about soil moisture content during rainy and dry seasons, Total-N, -P, -K from litter on different types of shade and age of coffee plants, and their effect on soil Available-N, -P, and -K. There are P1 (control), P2 (4-year-coffee + pine), P3 (7-year-coffee + pine), P4 (4-year-coffee + mahogany), and P5 (7-year-coffee + mahogany). These treatments affected to total soil moisture storage, Total-N, -P, -K of litter, and Available-N, -P, -K in the soil. The soil moisture storage change between rainy and dry seasons was 36.97 mm. The highest Total-N, -P, and -K of litter was 11.00 kg ha-1 y-1 at P3, 1.06 kg ha-1 y-1 at P2, and 4.35 kg ha-1 y-1 at P3, which was inconsistently associated with high soil nutrients. The highest Total-N was 0.40 (0-20 cm), 0.27 (20-40 cm), 0.30% (40-60 cm) at P4, Available-K was 1.69 (0-20 cm), 1.64 (20-40 cm), 1.87 cmol kg-1 (40-60 cm) at P5, and Available-P was 15.21 (0-20 cm), 14.06 (20-40 cm), 12.64 mg kg-1 (40-60 cm) at P1.
ANALISIS KAPASITAS INFILTRASI LAHAN PERTANIAN DI SUB DAS KALISARI, MALANG Nita, Istika; Ayuningtyas, Priska; Prijono, Sugeng; Putra, Aditya Nugraha
Jurnal Tanah dan Sumberdaya Lahan Vol. 11 No. 1 (2024)
Publisher : Departemen Tanah, Fakultas Pertanian, Universitas Brawijaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21776/ub.jtsl.2024.011.1.13

Abstract

Watershed hydrological conditions can decrease due to changes in land use and inappropriate land management. One of the watershed functions is providing water availability for agricultural areas. Along with the increasing area of agricultural land, there is often the issue of water availability, which has implications for the low opportunity for plants to use it. Infiltration is the initial process of water entry into the soil, so the availability of water is greatly influenced by this process. Agricultural land in the Kalisari sub-watershed is dry land and is dominated by dry fields. The area of the Kalisari sub-watershed has an area of ±5,000 ha divided into 5 land uses, namely mahogany-coffee agroforestry, pine-coffee agroforestry, scrub, dry land, and paddy fields. Infiltration measurements were spread over 43 measurement points, with the observed parameters being texture, bulk density, porosity, permeability, aggregate stability, and soil organic matter. The infiltration rate for all land uses is very fast (>25 cm hour-1), ranging from 12.00 cm hour-1 to 74.37 cm hour-1. The infiltration rate for all land uses was not significantly different; this was in line with soil properties, which included texture, bulk density (0.61-1.02 g cm-3), porosity (51.02-68.06%), permeability (4.88–6.79 cm hour-1), aggregate stability (2.11–3.34 mm), and organic matter (1.61-4.06%). However, the infiltration rate at the study site had a significant relationship with clay (r = -0.77), sand (r = 0.64), silt (r = 0.52) and soil organic matter   (r = 0.48).
Co-Authors A Ariffin Adinda Ardana Reswari Aditya Nugraha Putra, Aditya Nugraha Akmaludin Dimas Anggara Anis Nur Afifah Atiqah Aulia Hanuf Awal Maulana Faiz Ayuningtyas, Priska Azurianti Azurianti Beauty Laras Setia Pertiwi buhari umasugi Desya Wahyu Annisa Didik Suprayogo Dina Ananda Harfia Endah Umu Nur Holisah Husni Thamrin Sebayang Ieke Wulan Ayu Ika Lestiana Sari Istika Nita Iva Dewi Lestariningsih M Mashudi M Maswar Moh Harrys Pramudita Moh. Harrys Moh. Teguh Satya Laksmana Ni Made Sri Gitalaxmi Mahasidhi Rani Sahfitri Rensy Faradina Hikmawati Retno Suntari Rizki Puspita Rahmawati S Soemarno S Soemarno sa'diyah, zenny faridatus Salma J Fitra Saputra, Iwan Sarifudin Lathif Soemarno Soemarno Soemarno Soemarno Soemarno Srida Mitra Ayu Syafitri Dewi Widyantika Syaifuddin Iskandar Syawaluddin Akbar Ustiatik, Reni Wahid Wahid Wahyuni Setyo Lestari Wani Hadi Utomo Witno Witno Wulansari D. Nurrohmah Yazid Abdur Rahman Yulfita Farni Yulia Nuraini Yumna Yumna Zaenal Kusuma Zaenal Kusuma Zaenal Kusuma zenny faridatus sa'diyah