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Effect of water deficit of Ultisols, Entisols, Spodosols, and Histosols on oil palm productivity in Central Kalimantan

SAINS TANAH - Journal of Soil Science and Agroclimatology · Vol. 19 No. 2 (2022) · hlm. 180–191

DOI
10.20961/stjssa.v19i2.65455
ISSN
2356-1424, 1412-3606
Terbit
2022-12-29
Penerbit
Universitas Sebelas Maret
Bahasa
en

Abstrak

The same rainfall can cause different degrees of water stress depending on soil type, so the production response shown by plants can be different. This study is essential for growers, especially in predicting oil palm production based on water deficit for each soil type. The study was conducted on oil palm plantations in Central Kalimantan, Indonesia, with four soil types in 1,446.15 ha (40 blocks). The source of data collected from oil palm plantations included bunch number, average bunch weight, rainfall, and soil physical and chemical properties for the last 15 years (2007 - 2021). This experimental study used a two-stage cluster sampling method. The results showed that the best productivity, bunch number, and average bunch weight were found on Ultisols. The four soil types tested showed the same annual production distribution dynamic, but the response rate from each soil type showed differences. Entisols and Spodosols were more prone to drought stress due to water deficit than Ultisols and Histosols because of the differences in soil texture. Water deficit causes a decrease in oil palm productivity by 5 - 22% in the first year (Ultisols 12 - 22%; Entisols 12 - 22%; Spodosols 7 - 19%;Â Histosols 5 - 15%) and 1 - 8% in the second year (Ultisols 3 - 7%; Entisols 2 - 4%; Spodosols 5 - 8%; Histosols 1 - 5%) compared to previous years production. A decrease in oil palm productivity occurs at 3 - 5 months (bunch failure phase), 1 year (abortion sensitive phase), and 2 - 2.5 years (sex differentiation phase) after a water deficit appears.

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  • International Islamic University, Islamabad
  • Universitas Halu Oleo
  • Sunan Kalijaga State Islamic University Yogyakarta
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Rekan penulisOrganisasiArtikel bersama
Khoirudin khoirudinAfiliasi tidak diketahui5
Amri AbdulahAfiliasi tidak diketahui4
Apang Djafar ShieddiequeAfiliasi tidak diketahui3
Nourma Al ViandariAfiliasi tidak diketahui3
Nazar FazrinAfiliasi tidak diketahui3
Nana RahdianaAfiliasi tidak diketahui3
Rachmat Abdul GaniAfiliasi tidak diketahui3
Choirul AnwarInternational Islamic University, Islamabad2
Dede Ardi RajabAfiliasi tidak diketahui2
Yulfian AminandaAfiliasi tidak diketahui2
Basuki SumawinataAfiliasi tidak diketahui2
Heru Bagus PulunggonoAfiliasi tidak diketahui2
Anicetus WihardjakaAfiliasi tidak diketahui2
Muhamad Taufik UlhakimAfiliasi tidak diketahui2
Tomas IrfaniAfiliasi tidak diketahui2
Afif HakimAfiliasi tidak diketahui2
Amir AmirUniversitas Halu Oleo2
Renata Lintang AzizahAfiliasi tidak diketahui2
Yiyi SulaemanAfiliasi tidak diketahui2
Edi YatnoAfiliasi tidak diketahui2
Subaidi SubaidiSunan Kalijaga State Islamic University Yogyakarta1
Muhammad KhoiruddinAfiliasi tidak diketahui1
Mohamad Rifqi RoosdhaniAfiliasi tidak diketahui1
Abdulaziz KalupaeAfiliasi tidak diketahui1
Ibrahim TehhaeeAfiliasi tidak diketahui1
Noorsafuan Bin Che Noh FeloAfiliasi tidak diketahui1
Rila Rahma AprianiAfiliasi tidak diketahui1
Agung NugrohoAfiliasi tidak diketahui1
Joko PurnomoAfiliasi tidak diketahui1
Anhar AnharAfiliasi tidak diketahui1
Muhammad Darwis DasopangAfiliasi tidak diketahui1
Zainal Efendi HasibuanAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://jurnal.uns.ac.id/tanah/oai, pertama di-harvest 10 Nov 2026, terakhir terlihat 10 Nov 2026.
Metadata asli (oai_dc) 
<oai_dc:dc xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/  http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
	<dc:title xml:lang="en">Effect of water deficit of Ultisols, Entisols, Spodosols, and Histosols on oil palm productivity in Central Kalimantan</dc:title>
	<dc:creator xml:lang="en">Sukarman, Sukarman</dc:creator>
	<dc:creator xml:lang="en">Saidy, Akhmad R.</dc:creator>
	<dc:creator xml:lang="en">Rusmayadi, Gusti</dc:creator>
	<dc:creator xml:lang="en">Adriani, Dewi Erika</dc:creator>
	<dc:creator xml:lang="en">Primananda, Septa</dc:creator>
	<dc:creator xml:lang="en">Suwardi, Suwardi</dc:creator>
	<dc:creator xml:lang="en">Wirianata, Herry</dc:creator>
	<dc:creator xml:lang="en">Fitriana, Cindy Diah Ayu</dc:creator>
	<dc:subject xml:lang="en">Elaeis guineensis Jacq</dc:subject>
	<dc:subject xml:lang="en">Oil palm</dc:subject>
	<dc:subject xml:lang="en">Productivity</dc:subject>
	<dc:subject xml:lang="en">Soil types</dc:subject>
	<dc:subject xml:lang="en">Water deficit</dc:subject>
	<dc:description xml:lang="en">The same rainfall can cause different degrees of water stress depending on soil type, so the production response shown by plants can be different. This study is essential for growers, especially in predicting oil palm production based on water deficit for each soil type. The study was conducted on oil palm plantations in Central Kalimantan, Indonesia, with four soil types in 1,446.15 ha (40 blocks). The source of data collected from oil palm plantations included bunch number, average bunch weight, rainfall, and soil physical and chemical properties for the last 15 years (2007 - 2021). This experimental study used a two-stage cluster sampling method. The results showed that the best productivity, bunch number, and average bunch weight were found on Ultisols. The four soil types tested showed the same annual production distribution dynamic, but the response rate from each soil type showed differences. Entisols and Spodosols were more prone to drought stress due to water deficit than Ultisols and Histosols because of the differences in soil texture. Water deficit causes a decrease in oil palm productivity by 5 - 22% in the first year (Ultisols 12 - 22%; Entisols 12 - 22%; Spodosols 7 - 19%;  Histosols 5 - 15%) and 1 - 8% in the second year (Ultisols 3 - 7%; Entisols 2 - 4%; Spodosols 5 - 8%; Histosols 1 - 5%) compared to previous years production. A decrease in oil palm productivity occurs at 3 - 5 months (bunch failure phase), 1 year (abortion sensitive phase), and 2 - 2.5 years (sex differentiation phase) after a water deficit appears.</dc:description>
	<dc:publisher xml:lang="en">Universitas Sebelas Maret</dc:publisher>
	<dc:date>2022-12-29</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jurnal.uns.ac.id/tanah/article/view/65455</dc:identifier>
	<dc:identifier>10.20961/stjssa.v19i2.65455</dc:identifier>
	<dc:source xml:lang="en">SAINS TANAH - Journal of Soil Science and Agroclimatology; Vol. 19 No. 2 (2022): December; 180-191</dc:source>
	<dc:source>2356-1424</dc:source>
	<dc:source>1412-3606</dc:source>
	<dc:source>10.20961/stjssa.v19i2</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://jurnal.uns.ac.id/tanah/article/view/65455/38643</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2022 Sukarman, Akhmad R. Saidy, Gusti Rusmayadi, Dewi Erika Adriani, Septa Primananda, Suwardi,  Herry Wirianata, Cindy Diah Ayu Fitriana</dc:rights>
</oai_dc:dc>