scholarly journals Analysis and substantiation of methods for determining water consumption of haip-pasture herbs in conditions of irrigation by raining

2021 ◽  
pp. 93-97
Author(s):  
N. N. Dubenok ◽  
D. V. Yalansky ◽  
Yu. A. Mazhaysky ◽  
O. V. Chernikova ◽  
Yu. N. Dubrova
Keyword(s):  
Water Balance ◽  
Water Consumption ◽  
Weather Conditions ◽  
Balance Method ◽  
Moisture Capacity ◽  
Pasture Grass ◽  
Growing Seasons ◽  
Water Balance Method ◽  
Air Temperatures ◽  
The Republic

Relevance. The most important element of the operational regime of irrigation is the correct (timely) appointment and timing of irrigation, taking into account the biological characteristics of crops, weather conditions and the mechanical composition of the soil.Methods. In this work, the results of the calculation of the irrigation regime of the hay-pasture grass mixture for the growing season april-october 2016-2018 were presented, on the basis of which the values of the water consumption of the crop, the average values of bioclimatic and biothermal coefficients in relation to sod-podzolic loamy soils in the northeastern zones of the Republic of Belarus. The calculations were carried out by the water balance method, as well as by the method of maximum daily air temperatures.Results. As a result of calculating bioclimatic and biothermal coefficients and values of water consumption for the growing seasons. It was found that their highest values in all years of research were recorded in the variant with a pre-irrigation humidity level of 80% of the lowest moisture capacity, while their lowest values were observed in the variant with natural humidification. At the same time, as a result of calculations, it was established that the highest values of bioclimatic coefficients corresponding to the variant 80% of HB took the following values: 0.88; 0.72 and 0.66, the smallest are 0.71; 0.64 and 0.50, and the largest values of the biothermal coefficients were: 0.13; 0.15 and 0.15, the smallest are 0.09; 0.13 and 0.10, respectively, for the growing seasons. The largest values of water consumption, calculated by the water balance method, corresponding to the option 80% of the HB took the following values: 423.0; 462.0 and 440.0 mm, the smallest in this case were: 334.0; 404.0; and 331.0 mm, and the highest values of water consumption, calculated by the method of maximum daily temperatures were: 439.4; 420.0 and 432.2, while the smallest were equal: 318.7, 396.4 and 325.7 mm, respectively, for the growing seasons. 

Irrigation regime and water consumption of potatoes in the Republic of Bashkortostan, depending on the reclamation condition of lands

2020 ◽  
Vol 0 (6) ◽  
pp. 13-19
Author(s):  
Guzel Gumerova ◽  
Georgiy Gulyuk ◽  
Dmitry Kucher ◽  
Anatoly Shuravilin ◽  
Elena Piven
Keyword(s):  
Water Consumption ◽  
Weather Conditions ◽  
Growing Season ◽  
Vegetation Period ◽  
Forest Steppe ◽  
Total Water ◽  
Total Water Consumption ◽  
Republic Of Bashkortostan ◽  
Irrigated Lands ◽  
The Republic

Data of long-term researches (2015–2018) in southern forest-steppe zone of the Republic of Bashkortostan, is justified theoretically and experimentally the mode of irrigation of potatoes on leached chernozems of unsatisfactory, satisfactory and good ameliorative condition of irrigated lands. For the growing periods of potatoes with different heat and moisture supply, the number of watering, the timing of their implementation, irrigation and irrigation norms are established. On lands with unsatisfactory meliorative state the number of irrigation depending on weather conditions of potato vegetation period varied from 0 to 3 (1.5 on average) with average irrigation norm – 990 m3/ha. With satisfactory meliorative state of lands the number of irrigation on average increased from 0 to 4 (2.3 on average) with irrigation norm – 1305 m3/ha. On lands with good meliorative state the number of irrigation was the highest – from 1 to 5 (3 on average) with average irrigation irrigation norm is 1653 m3/ha. It was noted that in the dry periods of potato vegetation the greatest number of watering was carried out (3–5 watering), and in the wet periods (2017) watering was not carried out except for the area with a good reclamation state, where only one irrigation was carried out by the norm of 550 m3/ha. Water consumption of potato was studied in dynamics as a whole during the growing season and the months of the growing season depending on weather conditions of vegetation period and land reclamation condition of irrigated lands, as well as in the control (without irrigation). The lowest total water consumption was in the area without irrigation and averaged 226.8 mm. In irrigated areas, its values increased to 319-353.4 mm. The average daily water consumption varied from 2.12 to 3.3 mm. The highest rates of potato water consumption were observed in June and July, and the lowest – in May and August. In the total water consumption of potatoes on the site without irrigation, the largest share was occupied by atmospheric precipitation and in addition to them the arrival of moisture from the soil. Irrigation water was used in irrigated areas along with precipitation, the share of which was 30.2–46.1 %.

scholarly journals A worldwide evaluation of basin-scale evapotranspiration estimates against the water balance method

2016 ◽  
Vol 538 ◽  
pp. 82-95 ◽  
Author(s):  
Wenbin Liu ◽  
Lei Wang ◽  
Jing Zhou ◽  
Yanzhong Li ◽  
Fubao Sun ◽  
...  
Keyword(s):  
Water Balance ◽  
Balance Method ◽  
Water Balance Method ◽  
Basin Scale

scholarly journals Identification of the Impacts of Climate Changes and Human Activities on Runoff in the Jinsha River Basin, China

2017 ◽  
Vol 2017 ◽  
pp. 1-9 ◽  
Author(s):  
Xiaowan Liu ◽  
Dingzhi Peng ◽  
Zongxue Xu
Keyword(s):  
Water Balance ◽  
River Basin ◽  
Human Activities ◽  
Climate Changes ◽  
Balance Method ◽  
Variation Method ◽  
Rainfall Runoff ◽  
Jinsha River ◽  
Water Balance Method ◽  
Double Mass

Quantifying the impacts of climate changes and human activities on runoff has received extensive attention, especially for the regions with significant elevation difference. The contributions of climate changes and human activities to runoff were analyzed using rainfall-runoff relationship, double mass curve, slope variation, and water balance method during 1961–2010 at the Jinsha River basin, China. Results indicate that runoff at upstream and runoff at midstream are both dominated by climate changes, and the contributions of climate changes to runoff are 63%~72% and 53%~68%, respectively. At downstream, climate changes account for only 13%~18%, and runoff is mainly controlled by human activities, contributing 82%~87%. The availability and stability of results were compared and analyzed in the four methods. Results in slope variation, double mass curve, and water balance method except rainfall-runoff relationship method are of good agreement. And the rainfall-runoff relationship, double mass curve, and slope variation method are all of great stability. The four methods and availability evaluation of them could provide a reference to quantification in the contributions of climate changes and human activities to runoff at similar basins in the future.

scholarly journals Evaluation of Evapotranspiration Estimates in the Yellow River Basin against the Water Balance Method

Water ◽  
2018 ◽  
Vol 10 (12) ◽  
pp. 1884 ◽  
Author(s):  
Guojie Wang ◽  
Jian Pan ◽  
Chengcheng Shen ◽  
Shijie Li ◽  
Jiao Lu ◽  
...  
Keyword(s):  
Water Balance ◽  
River Basin ◽  
Land Surface ◽  
Yellow River ◽  
Yellow River Basin ◽  
Balance Method ◽  
The Yellow River ◽  
Water Balance Method ◽  
Global Land ◽  
The Yellow River Basin

Evapotranspiration (ET), a critical process in global climate change, is very difficult to estimate at regional and basin scales. In this study, we evaluated five ET products: the Global Land Surface Evaporation with the Amsterdam Methodology (GLEAM, the EartH2Observe ensemble (E2O)), the Global Land Data Assimilation System with Noah Land Surface Model-2 (GLDAS), a global ET product at 8 km resolution from Zhang (ZHANG) and a supplemental land surface product of the Modern-ERA Retrospective analysis for Research and Applications (MERRA_land), using the water balance method in the Yellow River Basin, China, including twelve catchments, during the period of 1982–2000. The results showed that these ET products have obvious different performances, in terms of either their magnitude or temporal variations. From the viewpoint of multiple-year averages, the MERRA_land product shows a fairly similar magnitude to the ETw derived from the water balance method, while the E2O product shows significant underestimations. The GLEAM product shows the highest correlation coefficient. From the viewpoint of interannual variations, the ZHANG product performs best in terms of magnitude, while the E2O still shows significant underestimations. However, the E2O product best describes the interannual variations among the five ET products. Further study has indicated that the discrepancies between the ET products in the Yellow River Basin are mainly due to the quality of precipitation forcing data. In addition, most ET products seem to not be sensitive to the downward shortwave radiation.

scholarly journals Sugar cane crop coefficient by the soil water balance method

2015 ◽  
Vol 10 (24) ◽  
pp. 2407-2414 ◽  
Author(s):  
Greco de Guimaraes Cardoso Gabriel ◽  
Campos de Oliveira Renato ◽  
Batista Teixeira Marconi ◽  
Sergio Dorneles Milton ◽  
Marcos Oliveira Domingos Romenig ◽  
...  
Keyword(s):  
Water Balance ◽  
Soil Water ◽  
Sugar Cane ◽  
Crop Coefficient ◽  
Balance Method ◽  
Soil Water Balance ◽  
Water Balance Method

Serial water balance method for predicting leachate generation in landfills

2003 ◽  
Vol 21 (2) ◽  
pp. 127-136 ◽  
Author(s):  
Ma. Teresa Orta De Velásquez ◽  
Reynaldo Cruz-Rivera ◽  
Neftalí Rojas-Valencia ◽  
Ignacio Monje-Ramírez ◽  
Jorge Sánchez-GóMez
Keyword(s):  
Water Balance ◽  
Balance Method ◽  
Water Balance Method

Glacier Mass Balance and Catchment-Scale Water Balance in Bolivian Andes

2016 ◽  
Vol 11 (6) ◽  
pp. 1040-1051
Author(s):  
Tong Liu ◽  
◽  
Tsuyoshi Kinouchi ◽  
Javier Mendoza ◽  
Yoichi Iwami ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Water Balance ◽  
Mass Balance ◽  
Balance Method ◽  
Glacier Mass Balance ◽  
Runoff Coefficient ◽  
Study Region ◽  
Bolivian Andes ◽  
Water Balance Method ◽  
Volume Relationship

In investigating glacier mass balance and water balance at Huayna Potosi West, a glacierized basin in the Bolivian Andes (Cordillera Real), we used a remote sensing method with empirical area-volume relationships, a hydrological method with runoff coefficients, and water balance method. Results suggest that remote sensing method based on the glacier area from satellite images and area-volume relationships is too imprecise to use in performing analysis in short time intervals. Glacier mass balance obtained using a new area-volume relationship was, however, similar to that obtained by the water balance method, thus proving that the new area-volume relationship is reasonable to use for analyzing glaciers within a certain size range. The hydrological method with a runoff coefficient considered glacier as the only storage for saving or contributing to runoff and nonglacier area as the only source of evaporation. We applied a fixed runoff coefficient of 0.8 without considering wet or dry seasons in nonglacier areas – a method thus sensitive to meteorological and hydrological data. We also did not consider glacier sublimation. The water balance method is applicable to the study region and excelled other methods in terms of resolution, having no empirical coefficients, and considering sublimation and evaporation. Among its few limitations are possibly underestimating evaporation and runoff over nonglacier areas during wet months and thus possibly overestimating glacier contribution at mean time.

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