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Lag times as indicators of hydrological mechanisms responsible for NO$_3$-N flushing in a forested headwater catchment
ID
Lebar, Klaudija
(
Avtor
),
ID
Vidmar, Andrej
(
Avtor
),
ID
Bezak, Nejc
(
Avtor
),
ID
Rusjan, Simon
(
Avtor
)
PDF - Predstavitvena datoteka,
prenos
(2,38 MB)
MD5: D98A894272BD7559A15CD2A53C59EDD6
URL - Izvorni URL, za dostop obiščite
https://www.mdpi.com/2073-4441/12/4/1092
Galerija slik
Izvleček
Understanding the temporal variability of the nutrient transport from catchments is essential for planning nutrient loss reduction measures related to land use and climate change. Moreover, observations and analysis of nutrient dynamics in streams draining undisturbed catchments are known to represent a reference point by which human-influenced catchments can be compared. In this paper, temporal dynamics of nitrate-nitrogen (NO$_3$-N) flux are investigated on an event basis by analysing observed lag times between data series. More specifically, we studied lag times between the centres of mass of six hydrological and biogeochemical variables, namely discharge, soil moisture at three depths, NO$_3$-N flux, and the precipitation hyetograph centre of mass. Data obtained by high-frequency measurements (20 min time step) from 29 events were analysed. Linear regression and multiple linear regression (MLR) were used to identify relationships between lag times of the above-mentioned processes. We found that discharge lag time (LAG$_Q$) and NO$_3$-N flux lag time (LAG$_N$) are highly correlated indicating similar temporal response to rainfall. Moreover, relatively high correlation between LAG$_N$ and soil moisture lag times was also detected. The MLR model showed that the most descriptive variable for both LAG$_N$ and LAG$_Q$ is amount of precipitation. For LAG$_N$, the change of the soil moisture in the upper two layers was also significant, suggesting that the lag times indicate the primarily role of the forest soils as the main source of the NO$_3$-N flux, whereas the precipitation amount and the runoff formation through the forest soils are the main controlling mechanisms.
Jezik:
Angleški jezik
Ključne besede:
hydrological processes
,
soil moisture
,
precipitation
,
runoff
,
nitrate flux
,
forested catchment
,
time lag
Vrsta gradiva:
Članek v reviji
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
FGG - Fakulteta za gradbeništvo in geodezijo
Status publikacije:
Objavljeno
Različica publikacije:
Objavljena publikacija
Leto izida:
2020
Št. strani:
13 str.
Številčenje:
Vol. 12, iss. 4, art. 1092
PID:
20.500.12556/RUL-128465
UDK:
556
ISSN pri članku:
2073-4441
DOI:
10.3390/w12041092
COBISS.SI-ID:
9113441
Datum objave v RUL:
14.07.2021
Število ogledov:
1145
Število prenosov:
224
Metapodatki:
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Objavi na:
Gradivo je del revije
Naslov:
Water
Skrajšan naslov:
Water
Založnik:
Molecular Diversity Preservation International - MDPI
ISSN:
2073-4441
COBISS.SI-ID:
36731653
Licence
Licenca:
CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:
http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:
To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Začetek licenciranja:
12.04.2020
Sekundarni jezik
Jezik:
Slovenski jezik
Ključne besede:
hidrološki procesi
,
vlažnost tal
,
padavine
,
odtok
,
gozdnato porečje
,
čas zakasnitve
Projekti
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Program financ.:
PhD grant
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P2-0180
Naslov:
Vodarstvo in geotehnika: orodja in metode za analize in simulacije procesov ter razvoj tehnologij
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