Abstract

Water is a key volatile that provides insights into the initial stages of planet formation. The low water abundances inferred from water observations toward low-mass protostellar objects may point to a rapid locking of water as ice by large dust grains during star and planet formation. However, little is known about the water vapor abundance in newly formed planet-forming disks. We aim to determine the water abundance in embedded Keplerian disks through spatially-resolved observations of H218_2^{18}O lines to understand the evolution of water during star and planet formation. We present H218_2^{18}O line observations with ALMA and NOEMA millimeter interferometers toward five young stellar objects. NOEMA observed the 31,3_{1,3} - 22,02_{2,0} line (Eup_{\rm up} = 203.7 K) while ALMA targeted the 41,44_{1,4} - 32,13_{2,1} line (Eup_{\rm up} = 322.0 K). Water column densities are derived considering optically thin and thermalized emission. Our observations are sensitive to the emission from the known Keplerian disks around three out of the five Class I objects in the sample. No H218_2^{18}O emission is detected toward any of our five Class I disks. We report upper limits to the integrated line intensities. The inferred water column densities in Class I disks are N < 1015^{15} cm−2^{-2} on 100 au scales which include both disk and envelope. The upper limits imply a disk-averaged water abundance of ≲10−6\lesssim 10^{-6} with respect to H2_2 for Class I objects. After taking into account the physical structure of the disk, the upper limit to the water abundance averaged over the inner warm disk with T>T> 100 K is between 10−7^{-7} up to 10−5^{-5}. Water vapor is not abundant in warm protostellar envelopes around Class I protostars. Upper limits to the water vapor column densities in Class I disks are at least two orders magnitude lower than values found in Class 0 disk-like structures.

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