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<p>Understanding processes controlling stream nutrient dynamics over time is crucial for implementing effective management strategies to prevent water quality degradation. In this respect, the study of the nutrient concentration–discharge (<span class="inline-formula"><i>C</i></span>–<span class="inline-formula"><i>Q</i></span>) relationship during individual runoff events can be a valuable tool for extrapolating the hydrochemical processes controlling nutrient fluxes in streams. This study investigated nitrogen concentration dynamics during events by analyzing and interpreting the nitrogen <span class="inline-formula"><i>C</i></span>–<span class="inline-formula"><i>Q</i></span> relationship in a small Atlantic (NW Iberian Peninsula) rural catchment. To this end, nitrate (<span class="inline-formula">NO₃-N</span>) and total Kjeldahl nitrogen (TKN) concentrations were monitored at a high temporal resolution during 102 runoff events over a 6-year period. For each of the selected runoff events, <span class="inline-formula"><i>C</i></span>–<span class="inline-formula"><i>Q</i></span> response was examined visually for the presence and direction of hysteresis loops and classified into three types of responses, namely clockwise, counterclockwise, and no hysteresis. Changes in concentration (<span class="inline-formula">Δ<i>C</i></span>) and the hysteresis direction (<span class="inline-formula">Δ<i>R</i></span>) were used to quantify nitrogen (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn></msub><mo>-</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="30pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ef11a71f7f4417b0142c7bf7895a70d8"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-27-1243-2023-ie00001.svg" width="30pt" height="15pt" src="hess-27-1243-2023-ie00001.png"/></svg:svg></span></span> and TKN) patterns during the runoff events. The transport mechanisms varied between compounds. The most frequent hysteretic response for <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn></msub><mo>-</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="30pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="eeef9b5ab0cce739a25a7a1797ec825b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-27-1243-2023-ie00002.svg" width="30pt" height="15pt" src="hess-27-1243-2023-ie00002.png"/></svg:svg></span></span> was counterclockwise with enrichment. On the contrary, the main TKN dynamic was enrichment with clockwise hysteresis. Event characteristics, such as rainfall amount, peak discharge (i.e., maximum discharge of the runoff event), and event magnitude relative to the initial baseflow (i.e., the difference between the maximum discharge of the runoff event and the initial baseflow divided by initial baseflow) provided a better explanation for hysteresis direction and magnitude for TKN than antecedent conditions (antecedent precipitation and baseflow at the beginning of the event). For <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M12" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn></msub><mo>-</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="30pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="a55c7f68d224cb7e4a0e12eba6d25ce4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-27-1243-2023-ie00003.svg" width="30pt" height="15pt" src="hess-27-1243-2023-ie00003.png"/></svg:svg></span></span> hysteresis, the role of hydrometeorological conditions was more complex. The <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M13" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn></msub><mo>-</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="30pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ebc779b72be81bc05a030550107b64bf"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-27-1243-2023-ie00004.svg" width="30pt" height="15pt" src="hess-27-1243-2023-ie00004.png"/></svg:svg></span></span> hysteresis magnitude was related to the magnitude of the event relative to the initial baseflow and the time elapsed since a preceding runoff event. These findings could be used as a reference for the development of N mitigation strategy in the region.</p>