izpis_h1_title_alt

Lag times as indicators of hydrological mechanisms responsible for NO$_3$-N flushing in a forested headwater catchment
ID Lebar, Klaudija (Author), ID Vidmar, Andrej (Author), ID Bezak, Nejc (Author), ID Rusjan, Simon (Author)

.pdfPDF - Presentation file, Download (2,38 MB)
MD5: D98A894272BD7559A15CD2A53C59EDD6
URLURL - Source URL, Visit https://www.mdpi.com/2073-4441/12/4/1092 This link opens in a new window

Abstract
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.

Language:English
Keywords:hydrological processes, soil moisture, precipitation, runoff, nitrate flux, forested catchment, time lag
Work type:Article
Typology:1.01 - Original Scientific Article
Organization:FGG - Faculty of Civil and Geodetic Engineering
Publication status:Published
Publication version:Version of Record
Year:2020
Number of pages:13 str.
Numbering:Vol. 12, iss. 4, art. 1092
PID:20.500.12556/RUL-128465 This link opens in a new window
UDC:556
ISSN on article:2073-4441
DOI:10.3390/w12041092 This link opens in a new window
COBISS.SI-ID:9113441 This link opens in a new window
Publication date in RUL:14.07.2021
Views:917
Downloads:191
Metadata:XML RDF-CHPDL DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a journal

Title:Water
Shortened title:Water
Publisher:Molecular Diversity Preservation International - MDPI
ISSN:2073-4441
COBISS.SI-ID:36731653 This link opens in a new window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.
Licensing start date:12.04.2020

Secondary language

Language:Slovenian
Keywords:hidrološki procesi, vlažnost tal, padavine, odtok, gozdnato porečje, čas zakasnitve

Projects

Funder:ARRS - Slovenian Research Agency
Funding programme:PhD grant

Funder:ARRS - Slovenian Research Agency
Project number:P2-0180
Name:Vodarstvo in geotehnika: orodja in metode za analize in simulacije procesov ter razvoj tehnologij

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back