Please use this identifier to cite or link to this item:https://hdl.handle.net/20.500.12259/90051
Type of publication: Straipsnis recenzuojamoje užsienio tarptautinės konferencijos medžiagoje / Article in peer-reviewed foreign international conference proceedings (P1d)
Field of Science: Aplinkos inžinerija / Environmental engineering (T004)
Author(s): Taparauskienė, Laima;Tanaskovik, Vjekoslav;Miseckaitė, Otilija;Adamonytė, Inga;Burbulis, Natalija
Title: Recommendations for agricultural drought assessment under Lithuanian climatic conditions
Is part of: ISAF 2015 [elektroninis išteklius] : 2nd International symposium for agriculture and food, 7-9 October 2015, Ohrid, Republic of Macedonia : symposium proceedings. Vol. 2 / Skopje : Faculty of Agricultural Sciences and Food, 2016
Extent: p. 613-621
Date: 2015
Keywords: Drought;Precipitation;Watermark;Plant stress
ISBN: 9789989845642
Abstract: Among the environmental stresses, drought stress is one of the most adverse factors that negatively impacts plant growth and productivity. Therefore, understanding and qualifying drought occurrence and its consequences on agricultural production, hydrologic cycle, and ecosystems is of particular importance. In the context of climate variability and change, water scarcity and food security, it is important to use more comprehensive data on rainfall, temperature and soils in computing drought indices. Currently for drought monitoring different indices, easily understandable, are used by end users. The Standardized Precipitation Index (SPI) was proposed by McKee et al. (1993) and it has been increasingly used during the last decades because of its solid theoretical development, robustness and versatility in drought analyses. Nevertheless for many years, the humidity of vegetation period has been described using Selyaninov's hydrothermal coefficient (HTK) in Lithuania. According to Farrago's classification, it belongs to drought indices of water balance group "supply/demand" as it uses daily values of precipitation and air temperature for the calculation of the period. Anyway drought affects water availability not only by changing regional precipitation level and temporal variability, but also by affecting water flows and soil moisture dynamics. Therefore it is essential lo have soil moisture data as one of the most important factors for evaluation of drought occurrence. Finally when all meteorological data are observed and soil moisture is monitored it is very important lo know what stress reaction of plants is. Results of investigation revealed a very strong negative relationship between soil moisture water content and proline content as well as between soil moisture water content and soluble sugar content in leaves
Internet: http://www.fznh.ukim.edu.mk/images/stories/symposium_proceedings_2015/02_symposium_proceedings_vol_ii.pdf
http://www.fznh.ukim.edu.mk/images/stories/symposium_proceedings_2015/02_symposium_proceedings_vol_ii.pdf
Affiliation(s): Vytauto Didžiojo universitetas
Žemės ūkio akademija
Appears in Collections:Universiteto mokslo publikacijos / University Research Publications

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