The responses of microbial communities in hyporheic zone to the eco-hydrological process
have been a hotspot in river ecological health research. However, the impact of different …

The carbonate critical zone (CZ) is characterized by extensive groundwater-surface water
exchange that leads to highly variable redox states of groundwater. Changes in redox …

The interfaces between rivers and aquifers are characterized by high spatial and temporal
variation in water flow, heat exchange, biogeochemical activity, and microbial and metazoan …

Rivers and streams are control points for CO2 emission to the air (fCO2), with emission rates
often exceeding internal metabolism (net ecosystem production, NEP). The difference is …

Water quantity and quality in karst aquifers may depend on decadal-scale variations in
recharge or withdrawal, which we hypothesize could be assessed through time-series …

Groundwater (GW) seepage can provide a major source of water, solutes, and contaminants
to rivers, but identifying magnitudes, directions and locations of seepage is complicated by …

Hydraulic properties such as stage and residence time are important controls on riverine N
removal. In most rivers, these hydraulic properties vary with stochastic precipitation forcing …

Aquatic N cycling arises from multiple overlapping and interacting pathways. In lotic
ecosystems, time-varying upstream delivery complicates isolation of internal …

江汉平原浅层地下水中锰含量普遍较高, 探究锰在河流交互带中的分布特征有助于认识交互带中
锰的生物地球化学过程, 对水质的保护具有重要指导意义. 通过监测汉江下游侧向交互带河水 …

ABSTRACT Groundwater (GW)–surface water (SW) interactions profoundly impact aquatic
systems. In karst regions characterized by the coexistence of various media, the hyporheic …