Stable Isotope Ratios in Tap Water of a Riverside City in a Semi-Arid Climate: An Application to Water Source Determination

Stable isotopes (e.g., <i>&#948;</i><sup>2</sup>H and <i>&#948;</i><sup>18</sup>O) in tap water are important tools to understand the local climate or environment background, water sources and the state of regional water supply. Based on 242 ta...

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Bibliographic Details
Main Authors: Mingxia Du, Mingjun Zhang, Shengjie Wang, Fenli Chen, Peipei Zhao, Su’e Zhou, Yaning Zhang
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/11/7/1441
Description
Summary:Stable isotopes (e.g., <i>&#948;</i><sup>2</sup>H and <i>&#948;</i><sup>18</sup>O) in tap water are important tools to understand the local climate or environment background, water sources and the state of regional water supply. Based on 242 tap water samples, 35 precipitation samples and 24 surface water samples gathered in the urban area of Lanzhou, the basic spatiotemporal characteristics of isotopes in tap water, their connection with isotopes in other water bodies and change during the process from raw water to tap water are discussed in detail, combining the information of local tap water supply and water source. It can provide reliable help for understanding the isotope characteristics of local tap water, regional water supply management and determination of tap water source of in a small area. Except for the establishment of a new data set of isotopes in tap water with complete time series and uniform spatial distribution of sampling sites, other results show that: (1) The Local Tap Water Line (LTWL) of Lanzhou is <i>&#948;</i><sup>2</sup>H = (6.03 &#177; 0.57) <i>&#948;</i><sup>18</sup>O + (&#8722;8.63 &#177; 5.44) (<i>r</i><sup>2</sup> = 0.41, <i>p</i> &lt; 0.01). (2) For seasonal variations, <i>&#948;</i><sup>2</sup>H and <i>&#948;</i><sup>18</sup>O in tap water both are higher in autumn and lower in spring. The diurnal and daily variations of isotopes in tap water are not large. As for spatial variations, the monthly mean values of <i>&#948;</i><sup>2</sup>H and <i>&#948;</i><sup>18</sup>O in tap water at each sampling site show little difference. The isotopes in tap water collected from one single sampling site can be considered as a representative for isotopes in tap water in the area with a single tap water source. (3) Isotopes in tap water show weak connection with precipitation isotopes, but exhibit good connection (consistent seasonal variation, similar numerical range, small numerical difference and high correlation) with isotopes in surface water, which is the direct water source. Isotopes in water change little from raw water to tap water. Isotopic composition of tap water in Lanzhou can be used as a representative of isotopes in surface water.
ISSN:2073-4441