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Robusta coffee transpiration rate in smallholder coffee plantations on Inceptisols of Malang, East Java

Journal of Degraded and Mining Lands Management · Vol. 9 No. 1 (2021) · hlm. 3165–3173

DOI
10.15243/jdmlm.2021.091.3165
ISSN
2502-2458, 2339-076X
Terbit
2021-10-01
Penerbit
Brawijaya University
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-nc/4.0

Abstrak

Climate change and the erratic and uneven rainfall distribution are the causes of reduced water available in the soil for plant needs to the transpiration process. This study aimed to determine coffee transpiration rate on dry land with rain harvesting techniques during the dry season, transition season, and rainy season and the factors that influence it. This study used field observation and laboratory analysis with two treatments, i.e. a bench terrace as a control (P1) and an L-shaped silt pit (P2). The variables observed were soil moisture content, transpiration rate, soil water potential, leaf water potential, and microclimate, especially temperature and sunlight intensity. The results showed that the transpiration rate of coffee plants was significantly different in the two treatments. The highest transpiration rate was found in P2 as much as 13.17 mm week-1 or equivalent to 1.88 mm day-1 during the dry season. Application of the L-shaped silt pit (P2) increased soil moisture content compared to the control (P1). This increase was followed by an increase in soil water potential and leaf water potential, which could reach the highest values of 0.18 bar and 0.49 bar, respectively. The transpiration decreases with the change of seasons from the dry season to the transitional season and the rainy season. This decrease is caused by changes in the microclimate, especially the temperature and sunlight intensity. Both are the most variables that affect the rate of transpiration.

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  • University of Brawijaya
  • Universitas Halu Oleo
  • Universitas Islam Malang
  • Yamaguchi University
  • Universitas Wisnuwardhana Malang
  • National Research and Innovation Agency
  • Malikussaleh University
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Rekan penulisOrganisasiArtikel bersama
Soemarno SoemarnoUniversity of Brawijaya4
Novi ArfaritaUniversitas Islam Malang4
Tsuyoshi ImaiYamaguchi University2
Zaenal KusumaUniversity of Brawijaya2
Atiqah Aulia HanufUniversity of Brawijaya2
Retno SuntariUniversity of Brawijaya2
Yulia NurainiUniversity of Brawijaya2
Sri Rahayu UtamiUniversity of Brawijaya2
Cahyo PrayogoUniversity of Brawijaya2
Christopher AndersonAfiliasi tidak diketahui1
Syahrul KurniawanUniversity of Brawijaya1
Ian A. NavaretteAfiliasi tidak diketahui1
Miftakhul MukharomahUniversity of Brawijaya1
Djuhari DjuhariUniversitas Islam Malang1
Dimas PrastyajiUniversity of Brawijaya1
Nurul MuddarisnaUniversitas Wisnuwardhana Malang1
H MelsandiUniversity of Brawijaya1
Ayyu RahayuNational Research and Innovation Agency1
C C WatiUniversity of Brawijaya1
H HafifahMalikussaleh University1
S SudiarsoUniversity of Brawijaya1
Mochammad Dawam MaghfoerUniversity of Brawijaya1
Didik SuprayogoUniversity of Brawijaya1
Moh. Teguh Satya LaksmanaUniversity of Brawijaya1
M MashudiAfiliasi tidak diketahui1
Buhari UmasugiKhairun University1
Ariff Ikhwan AriffinUniversity of Brawijaya1
Yulfita FarniUniversitas Jambi1
June Annethe PutinellaUniversitas Pattimura1
S SyarifinnurUniversity of Brawijaya1
Albasri AlbasriUniversitas Halu Oleo1
Husna HusnaUniversitas Halu Oleo1
Faisal Danu TuheteruUniversitas Halu Oleo1
Asrianti ArifUniversitas Halu Oleo1
Basrudin BasrudinUniversitas Halu Oleo1
Irdika MansurIPB University1
Maman TurjamanMinistry of Environment and Forestry, Republic of Indonesia1

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Sumber metadata: OAI-PMH (metadata jurnal) http://jdmlm.ub.ac.id/index.php/jdmlm/oai, pertama di-harvest 9 Nov 2026, terakhir terlihat 9 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-US">Robusta coffee transpiration rate in smallholder coffee plantations on Inceptisols of Malang, East Java</dc:title>
	<dc:creator>Saputri, Jiyanti Yana</dc:creator>
	<dc:creator>Prijono, Sugeng</dc:creator>
	<dc:creator>Prasetya, Budi</dc:creator>
	<dc:subject xml:lang="en-US">climate change</dc:subject>
	<dc:subject xml:lang="en-US">leaf water potential</dc:subject>
	<dc:subject xml:lang="en-US">soil moisture content</dc:subject>
	<dc:subject xml:lang="en-US">soil water potential</dc:subject>
	<dc:subject xml:lang="en-US">transpiration</dc:subject>
	<dc:description xml:lang="en-US">Climate change and the erratic and uneven rainfall distribution are the causes of reduced water available in the soil for plant needs to the transpiration process. This study aimed to determine coffee transpiration rate on dry land with rain harvesting techniques during the dry season, transition season, and rainy season and the factors that influence it. This study used field observation and laboratory analysis with two treatments, i.e. a bench terrace as a control (P1) and an L-shaped silt pit (P2). The variables observed were soil moisture content, transpiration rate, soil water potential, leaf water potential, and microclimate, especially temperature and sunlight intensity. The results showed that the transpiration rate of coffee plants was significantly different in the two treatments. The highest transpiration rate was found in P2 as much as 13.17 mm week-1 or equivalent to 1.88 mm day-1 during the dry season. Application of the L-shaped silt pit (P2) increased soil moisture content compared to the control (P1). This increase was followed by an increase in soil water potential and leaf water potential, which could reach the highest values of 0.18 bar and 0.49 bar, respectively. The transpiration decreases with the change of seasons from the dry season to the transitional season and the rainy season. This decrease is caused by changes in the microclimate, especially the temperature and sunlight intensity. Both are the most variables that affect the rate of transpiration.</dc:description>
	<dc:publisher xml:lang="en-US">Brawijaya University</dc:publisher>
	<dc:date>2021-10-01</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://jdmlm.ub.ac.id/index.php/jdmlm/article/view/998</dc:identifier>
	<dc:identifier>10.15243/jdmlm.2021.091.3165</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Degraded and Mining Lands Management; Vol. 9 No. 1 (2021); 3165-3173</dc:source>
	<dc:source>2502-2458</dc:source>
	<dc:source>2339-076X</dc:source>
	<dc:source>10.15243/jdmlm.2021.091</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/998/pdf</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2021 Journal of Degraded and Mining Lands Management</dc:rights>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-nc/4.0</dc:rights>
</oai_dc:dc>