Cold seeps with methane-rich fluids leaking out of the seafloor usually support massive
biomass of chemosynthetic organisms and associated fauna. A substantial amount of …

Dissolved organic matter (DOM) in surface waters can vary markedly in character depending
on seasonal variations such as rainfall intensity, UV radiations and temperature. Changes in …

Disinfection byproduct (DBP) formation, prediction, and minimization are critical challenges
facing the drinking water treatment industry worldwide where chemical disinfection is …

Aim The need to go beyond taxonomy to understand patterns in microbial function has led to
an increased use of trait‐based approaches, yet we know little about how microbial …

Duplicate, filtered samples of North Atlantic Deep Water (NADW) were irradiated for 28 days
in a solar simulator. Duplicate dark controls were placed alongside the irradiated samples …

Electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (ESI-
FTICR-MS) has proven to be a powerful technique revealing complexity and diversity of …

The fate of carbon stored in permafrost-zone peatlands represents a significant uncertainty
in global climate modeling. Given that the breakdown of dissolved organic matter (DOM) is …

Soils export large amounts of organic matter to rivers, and there are still major uncertainties
concerning the composition and reactivity of this material and its fate within the fluvial …

The adsorption of dissolved organic matter (DOM) to metal (oxy) hydroxide mineral surfaces
is a critical step for C sequestration in soils. Although equilibrium studies have described …

Dissolved organic matter (DOM) quantity and composition control the rate of formation (R f,
T) of triplet excited states of dissolved natural organic matter (3DOM*) and the efficiency of …