The terrestrial components of the hydrological cycle include rainwater, surface water, and
groundwater. Carbon (C) isotopes allow hydrologists to pinpoint the age of groundwater …

As the permafrost region warms and permafrost soils thaw, vast pools of soil organic carbon
(C) become vulnerable to enhanced microbial decomposition and lateral transport into …

This study investigates surface water contamination of Ben-Kazza River in Morocco, fed by
effluents from an adjacent lagoon-based wastewater treatment plant (WWTP) and …

Ratios of glycerol dialkyl glycerol tetraethers (GDGT), which are membrane lipids of bacteria
and archaea, are at the base of several paleoenvironmental proxies. They are frequently …

Dissolved organic carbon (DOC) flux from rivers in the pan‐Arctic watershed represents an
important connection between major terrestrial carbon stocks and the Arctic Ocean. Previous …

Rivers are the main way of mobilizing, transforming and transporting of dissolved organic
carbon to the ocean, thus largely determining the features of the carbon cycle on the Arctic …

Thawing Arctic permafrost can induce hydrologic change and alter redox conditions, shifting
the balance of soil organic matter (SOM) decomposition. There remains uncertainty about …

Dissolved organic matter (DOM) is a small but very reactive pool of organic matter (OM) in
the environment. Its role is related to its composition, which depends on its source. In soils …

Tropical soils play a critical role in the global biogeochemical cycles and are essential for
maintaining the Earth's carbon balance. Understanding the dynamics of dissolved organic …

Urbanization has notably changed the characteristics and functions of watershed
ecosystems worldwide, influencing the characteristics of chromophoric dissolved organic …