Hydropeaking as the most prominent feature of flow alterations resulting
from hydropower plants has received attention worldwide. Ramifications
of hydropower on the downstream river systems mainly focus on
hydrological regimes or long-term water quality changes. Exceptional
knowledge is expected on the sub-daily changes of water qualities in the
downstream river reach that is affected by the hydropeaking. In this
study, we investigate the dynamics of hydropeaking and thermopeaking at
the outlet of the Three Gorges Dam TGD using a high temporal resolution
dataset, and inspect its association with water chemistry indices.
Hourly measurements are analysed for the downstream station Yunchi , and
compared with the upstream station Nanjinguan. The results show that
along with water temperature, water quality indices such as dissolved
oxygen, total Phosphorus, total nitrogen, PH, and electricity
conductivity all show evident ‘peaking’ phenomenon in a short time.
These divergent variations, however, are not valid for non-hydropeaking
affected indicators including turbidity, permanganate index, and ammonia
nitrogen. These hydropeaking-induced perturbations are mitigated by the
flood control operation from July to September. This study demonstrates
that water quality indices are sensitive to hydropeaking and
thermopeaking with respect to the magnitude of change and the seasonal
component during a year. The results provide additional evidence for the
environmental impacts of hydropower regulation on the receiving river
reach, and bridge the gap between hydropeaking studies and
thermopeaking, and study water qualities variations that were seldom
connected from the same temporal perspective in river research.