# Deciphering CO2 flux and fluorescent DOM origins in the carbon cycle of Kaptai Lake

## TL;DR

This study analyzed water quality and CO2 flux in Kaptai Lake, finding it releases CO2 and identifying sources of organic matter.

## Contribution

The study provides new insights into CO2 flux and fDOM sources in Kaptai Lake using advanced optical and sensor techniques.

## Key findings

- Kaptai Lake acts as a net source of CO2 to the atmosphere with fluxes between 45 and 56 mmol CO2 m⁻² d⁻¹.
- Fluorescent DOM in the lake is primarily biologically derived and influenced by microbial processes.
- Spatial variability in fDOM suggests localized pollution sources affecting the lake's carbon cycle.

## Abstract

This study aimed to assess the current water quality, identify the sources of fluorescent dissolved organic matter (fDOM), and quantify the CO2 flux from Kaptai Lake surface water. A water quality multiparameter analyzer, a membrane-enclosed pCO2 sensor, and a weather monitoring device were deployed to continuously record data over 48 hours to observe daily and spatial shifts. All measured water quality parameters remained within the acceptable limits set by the Department of Environment (DoE). The three-dimensional excitation-emission matrix (3D-EEM) analysis identified distinct fluorophores at peak A (Ex/Em = 245/404 nm), peak M (Ex/Em = 310/404 nm), peak T (Ex/Em = 280/338–346 nm), and peak Tuv (Ex/Em = 230/338–350 nm). Parallel factor analysis (PARAFAC) modelling further resolved these into protein-like components and fulvic-like substances, specifically C-like and M-like fluorophores, indicating the presence of both microbial and terrestrial sources. Spatial distribution patterns of fDOM intensity suggest variability driven by localized pollution sources across the lake. Optical indices further indicated that the fDOM components were predominantly biologically derived, characterized by low aromaticity, lower molecular weight and size, and were largely influenced by microbial degradation processes. Diurnal monitoring of partial pressure of CO2 (pCO2) in the lake water revealed values ranging from 577 to 1045 µatm. Correspondingly, the CO2 flux (FCO2) varied between 45 and 56 mmol CO2 m ⁻ 2 d ⁻ 1. The positive average FCO₂ indicates that the lake acts as a net source of CO2 to the regional atmosphere. Higher pCO2 levels are linked to lower dissolved oxygen and increased protein-like DOM that fuels microbial respiration, while humic-like DOM helps stabilize carbon by limiting CO2 release.