Assessment of crop water requirement of capsicum chinense grown in a protected house: a stable water isotope based method

dc.contributor.authorTharundya, SAS
dc.contributor.authorPerera, RRUR
dc.contributor.authorEdirisinghe, EANV
dc.contributor.authorWithanage, NS
dc.contributor.authorAbhiram, G
dc.contributor.authorPriyadarshanee, S
dc.contributor.authorKalpage, M
dc.contributor.authorLiyanage, HPK
dc.contributor.editorRajapakse, RLHL
dc.contributor.editorPrasath, RA
dc.date.accessioned2026-11-03T10:14:23Z
dc.date.issued2026
dc.description.abstractSri Lanka is an agricultural country facing several challenges. One of them is that available accessible fresh water is limited for the crop fields. This study aimed to enhance the agronomic performance and Water Use Efficiency (WUE) of Scotch Bonnet (Capsicum chinense) under different irrigation levels in a protected house. The experiment was conducted using a Completely Randomized Design with three irrigation treatments and 12 replicates per treatment. Three irrigation treatments were implemented based on Total Available Water (TAW) and Allowable Depletion Levels of the potting mixture. Treatment 01 plot was maintained at 60% moisture of TAW, Treatment 02 at 40% and Treatment 03 at 25%. Once the specified depletion level was reached, each pot was irrigated according to the estimated Net Irrigation Requirement to reinstate soil moisture to Field Capacity. Growth parameters were measured weekly. Stable Water Isotopes were analyzed using water extracted from soil and leaf samples by Vacuum Cryogenic Extraction. WUE is calculated as the yield produced per unit of water used through evapotranspiration. The results revealed that, during transpiration, lighter isotopes (1H and 16O) leave the leaves more easily, while heavier isotopes (2H and 18O) became relatively enriched in leaves. Stable water isotopes extracted from leaf, soil, and atmospheric moisture samples formed three separate clusters around the Local Meteoric Water Line. Isotope data showed distinct signals from evaporation, transpiration, and evapotranspiration. WUE values for T1, T2, and T3 were 0.00058, 0.0017, and 0.0050 kg L⁻1, respectively. Overall T3 showed the best growth, yield, and WUE. These isotope differences helped distinguish evaporation from transpiration and explain water movement through the soil–plant–atmosphere system.
dc.identifier.conferenceICEWSE 2026- 2nd International Conference on Energy and Water for Sustainable Environment 2026
dc.identifier.departmentDepartment of Civil Engineering
dc.identifier.doihttps://doi.org/10.31705/ICEWSE.2026.39
dc.identifier.emailstharundya@gmail.com
dc.identifier.facultyEngineering
dc.identifier.issn3121-5599
dc.identifier.pgnos42 p.
dc.identifier.placeUniversity of Moratuwa, Sri Lanka
dc.identifier.proceedingBook of Abstracts of the 2nd International Conference on Energy and Water for Sustainable Environment 2026 (ICEWSE 2026)
dc.identifier.publisherUNESCO Madanjeet Singh Centre for South Asia Water Management (UMCSAWM)
dc.identifier.urihttps://dl.lib.uom.lk/handle/123/25855
dc.identifier.year2026
dc.language.isoen
dc.subjectAGRONOMIC PERFORMANCE
dc.subjectEVAPOTRANSPIRATION
dc.subjectSTABLE WATER ISOTOPES
dc.subjectVACUUM CRYOGENIC EXTRACTION
dc.subjectWATER USE EFFICIENCY
dc.titleAssessment of crop water requirement of capsicum chinense grown in a protected house: a stable water isotope based method
dc.typeConference-Abstract

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