Pregled bibliografske jedinice broj: 1197424
Utilizing Stable Water Isotopes (δ2H and δ18O) to Study Soil-Water Origin in Sloped Vineyard: First Results
Utilizing Stable Water Isotopes (δ2H and δ18O) to Study Soil-Water Origin in Sloped Vineyard: First Results // Rudarsko-geološko-naftni zbornik, 59 (2022), 3; 1-14 doi:10.17794/rgn.2022.3.1 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1197424 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Utilizing Stable Water Isotopes (δ2H and δ18O) to
Study Soil-Water Origin in Sloped Vineyard: First
Results
Autori
Zoran, Kovač ; Vedran, Krevh ; Lana, Filipović ; Jasmina, Defterdarović ; Patricia, Buškulić ; Luka, Han ; Vilim, Filipović
Izvornik
Rudarsko-geološko-naftni zbornik (0353-4529) 59
(2022), 3;
1-14
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
soil-water behaviour ; precipitation infiltration ; stable isotopes of water ; hillslope vineyard ; vadose zone
Sažetak
The diversity of processes taking place in hillslope agro-ecosystems makes the estimation of vadose zone dynamics rather challenging. This paper presents the first insight into the research of volumetric water content, granulometric composition, meteorological data, precipitation and soil-water isotopic composition conducted within the SUPREHILL project at its vadose zone observatory. The main goals of this research are related to the evaluation of soil-water origin at the hillslope vineyard, but also to the estimation of depths until which precipitation infiltrates and where the occurrence of preferential flow is possible. For that purpose, hydrometeorological data, granulometric composition and stable iso- topes of hydrogen (δ2H) and oxygen (δ18O) from precipitation and sampled soil water have been used. The results indi-cate the existence of a different isotopic signature in soil water, which suggests different infiltration patterns in the inves-tigated area. Also, the results point out that surface runoff, subsurface runoff, and most of the passive wick lysimeters respond to precipitation, while the response of suction probes located at deeper depth is not that evident. This corre-sponds to the results related to the variation of water content at different depths. All the results indicate the possible existence of a low permeable layer at an approximate depth of 60 cm. Furthermore, preferential flow, if it exists, can be expected from the shallowest depths of the vineyard to a maximum depth of 80 cm. It is expected that an established long-term monitoring network at the SUPREHILL Observatory will give a more precise definition of soil-water behaviour and the existence of preferential flow
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo, Poljoprivreda (agronomija), Interdisciplinarne biotehničke znanosti
POVEZANOST RADA
Projekti:
--UIP-2019-04-5409 - Podpovršinski preferencijalni transportni procesi u poljoprivrednim padinskim tlima (SUPREHILL) (Filipović, Vilim) ( CroRIS)
Ustanove:
Agronomski fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb
Profili:
Vilim Filipović
(autor)
Zoran Kovač
(autor)
Jasmina Defterdarović
(autor)
Lana Filipović
(autor)
Patricia Buškulić
(autor)
Vedran Krevh
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Emerging Sources Citation Index (ESCI)
- Scopus