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PERANAN MAKROFIT AIR Hydrilla verticillata (L. f.) Royle SEBAGAI PENYUMBANG OKSIGEN DI AIR GAMBUT PADA BEBERAPA TINGKAT BIOMASA DAN CAHAYA

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dc.contributor.author Fatonah, Siti
dc.contributor.author Muhammad, Ahmad
dc.contributor.author Zega, Shinta Ariani
dc.contributor.author Saputri, Dwijowati Asih
dc.date.accessioned 2020-10-06T05:17:40Z
dc.date.available 2020-10-06T05:17:40Z
dc.date.issued 2019-11
dc.identifier.isbn 978-60251349-1-3
dc.identifier.other wahyu sari yeni
dc.identifier.uri https://repository.unri.ac.id/handle/123456789/9860
dc.description.abstract Hydrilla verticillata are found in freshwater and peat waters. Light absorbed by macrophytes can be reduced because of suspended particles and the presence of shade from plants that are around the waters. The density of H. verticillata varies depending on environmental conditions. This study aims to determine the role of H. verticillata (L. f.) Royle water macrophytes as a contributor of oxygen in peat waters at various levels of H. verticillata and light densities. The study was conducted ex situ, by planting macrophytes in peat and fresh water in plastic containers under open and shade conditions. The research was Randomized Complete Block Design. H. Verticillata biomass, consisting of four levels, namely 0 g (without plants), 30 g (30% Hydrilla macrophytic closure for each volume of 5.5 liters), 60g (60%) and 90g (90%). The results showed that the content of dissolved oxygen in peat water was lower than that of fresh water. The presence of shade in peat or fresh water decreases the dissolved oxygen content. High increases in macrophytic biomass (60 and 90% closure) do not significantly increase DO. The presence of Hydrilla verticillata in peat water in open conditions can contribute dissolved oxygen around 0.93 to 1.38 mg / l with an increase percentage of 28 to 42%. In the shade conditions, the presence of H verticyllata macrophytes in peat water can contribute about 0.67 to 0.83 mg / l of dissolved oxygen with a percentage increase of 27 to 36% during the day. DO diurnal DO fluctuations occur in the morning (8:00), afternoon (12.00) and evening (16.00), with the highest DO content during the day. en_US
dc.description.provenance Submitted by Evi Susanti (repository@unri.ac.id) on 2020-10-06T05:17:40Z No. of bitstreams: 1 4. siti fatonah.pdf: 3290100 bytes, checksum: d3cd5fbddf37d1400c4eecb7eb6449dd (MD5) en
dc.description.provenance Made available in DSpace on 2020-10-06T05:17:40Z (GMT). No. of bitstreams: 1 4. siti fatonah.pdf: 3290100 bytes, checksum: d3cd5fbddf37d1400c4eecb7eb6449dd (MD5) Previous issue date: 2019-11 en
dc.description.sponsorship PROSIDING SENPLING 2019 “Konservasi Sumber Daya Alam Hayati dan Ekosistem Program Doktor Ilmu Lingkungan PPs UNRI Jl. Pattimura No. 09 Gobah-Pekanbaru Email: psil_unri@yahoo.com en_US
dc.language.iso en en_US
dc.subject biomass en_US
dc.subject dissolved oxygen en_US
dc.subject Hydrilla verticillata (L. f.) Royle en_US
dc.subject peat water en_US
dc.subject light en_US
dc.title PERANAN MAKROFIT AIR Hydrilla verticillata (L. f.) Royle SEBAGAI PENYUMBANG OKSIGEN DI AIR GAMBUT PADA BEBERAPA TINGKAT BIOMASA DAN CAHAYA en_US
dc.type Article en_US


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