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BY-NC-ND 3.0 license Open Access Published by De Gruyter Open Access February 29, 2016

Micro-scale hydrological field experiments in Romania

  • Gabriel Minea EMAIL logo and Gabriela A. Moroşanu
From the journal Open Geosciences

Abstract

The paper (communication) presents an overview of hydrologic field experiments at micro-scale in Romania. In order to experimentally investigate micro (plot)-scale hydrological impact of soil erosion, the National Institute of Hydrology and Water Management founded Voineşti Experimental Basin (VES) in 1964 and the Aldeni Experimental Basins (AEB) in 1984. AEB and VES are located in the Curvature Subcarpathians. Experimental plots are organized in a double systems and have an area of 80 m2 (runoff plots) at AEB and 300 m2 (water balance plots) at VES. Land use of plot: first plot ”grass-land” is covered with perennial grass and second plot (control) consists in ”bare soil”. Over the latter one, the soil is hoeing, which results in a greater development of infiltration than in the first plot. Experimental investigations at micro-scale are aimed towards determining the parameters of the water balance equation, during natural and artificial rainfalls, researching of flows and soil erosion processes on experimental plots, extrapolating relations involving runoff coefficients from a small scale to medium scale. Nowadays, the latest evolutions in data acquisition and transmission equipment are represented by sensors (such as: sensors to determinate the soil moisture content). Exploitation and dissemination of hydrologic data is accomplished by research themes/projects, year-books of basic data and papers.

1 Introduction

Experimentation and observations are leading activities within the water sciences [1]. From a hydrological point of view, experimental basins are typical natural laboratories, which play an important role in understanding the dynamics of genetic (natural or simulated rainfall) and conditional (soil, land use, vegetation type, human activity, etc.) factors that influence the overland flow and suspended load discharges. Moreover, plot-scale experimental studies are designed to improve our understanding of the relationships between processes involving hydrological, ecological and geomorphic factors [25].

Regarding water balance investigations, experimental studies at a hydrological micro-scale (1 cm2 → 1 km2) allow simulations of elementary hydrological processes by means of runoff plots [57]. The sizes of runoff plots are: (a) microplots (i.e. one or two square meters), (b) small-scale (i.e. ∼100 m2) and (c) field plots (i.e. ∼1 ha) [8]. Thus the results obtained are representative for a region or a certain conditional factor, and by means of extrapolation, these results can be used on the slopes of the catchment. Several types of studies can be used, such as: data modeling; assessing socio-economic impact aspects of the water resource; detection of trends and changes in runoff regimes and ecosystem responses due to human activities and climate variability [9]. In 1986 UNESCO created the Euro-Mediterranean Network of Experimental and Representative Basins (ERB), through its International Hydrological Program (IHP), and Romania has been affiliated with this organization since 1993, through the National Institute of Hydrology and Water Management (NIHWM). Within the NIHWM, experimental hydrological research on runoff plots, in correlation with complex programs of observations and measurements, is conducted at 2 research units. The content of its activity concerns the establishment of quantitatively defined relationships of runoff and genetic and conditional factors. These basins are situated in the Curvature Subcarpathians (Figure 1). The hydrologic activity started around 1964, with the founding of the Station for the Experimental Hydrology of Voineşti, now called Voineşti Experimental Basin, and since 1984 to Aldeni [10, 11]. On the basis of data obtained from these research units, especially those related to deterministic models, numerous studies have been published [10, 1218].

Figure 1 Geographical position of ALDENI and VOINEfiTI Experimental Basins.
Figure 1

Geographical position of ALDENI and VOINEfiTI Experimental Basins.

Within the Aldeni Experimental Basin and Voineşti Experimental Basin, the micro-scale study of hydrological components of the water budget is conducted using equipment that allows an estimation of the physiographic in-fluences in the region (geomorphic, climatic, soil) and anthropic intervention – land reclamation.

The objective of this paper is to present an overview about hydrometric equipment related to the hydrological field experiments research at micro-scale carried out by the National Institute of Hydrology and Water Management (Romania).

2 Material and methods

The main data used in this communication were the bibliographic and technical resources, as well as the hydrometeorological data (i.e. water discharge, rainfall). The method used in the study was based on the investigation of bibliographical resources and field observations. The mapping was made using ArcGIS Version 9.3 and the graphical representations of hydrometeorological data were performed using OriginPro version 8.5.

3 Results and discussion

3.1 Historical and geographical background

The National Institute of Hydrology and Water Management (NIHWM) began micro-scale, experimental research – with experimental plots – of the hydrological impacts of soil erosion and water balance in soil, in 1964 at the Station for Experimental Hydrology Voineşti (VES) and in 1984, at the Aldeni Experimental Basin (AEB).

3.2 Aldeni Experimental Basin

Studies in the AEB were conducted as part of comprehensive hydrologic research initiated in 1980. In the same year, the first field explorations were conducted and between 1981 and 1984, in collaboration with the present-day University of Agronomic Sciences and Veterinary Medicine of Bucharest, soil improvement activities were initiated (terracing, artificial rill and orchard planting), in order to assess, finalize and homologate the basin. Engineering works (e.g.: terraces) conducted by AEB, allowed water and suspended load discharge values determination in a modified regime.

In terms of geomorphology, AEB is situated in the Curvature Subcarpathians (45°19’30”N latitude and meridian 26°44’43”E longitude); a region characterized by intensive soil erosion – especially in the eastern part [19, 20]. Hydro-graphically, it forms part of the Slănic River Catchment, a left-side tributary of the Buzău River (Figure 1). The landscape presents torrential formations of different stages (rills, ephemeral gully, gully). The region has a moderate temperate-continental climate with „rainshadow” and dominance of dry winds coming down from the Carpathians. The mean annual precipitation of and mean annual temperature for the period 1984-2014 was 550 mm and 9.5°C respectively. In the study area, on runoff plots, the soil type is alluviosols with coluvic subtype; generally have clay content (36.5%), humus (3.28%), the phosphorus (24%) and ph = 7.2 – a neutral reaction – mildly alkaline [21]. Actual land use is in decline (typical perennial grass), due to partial abandonment and/or unproductive land.

3.3 Voineşti experimental basin

The Voineşti Experimental Basin (VEB) was created in 1963, though the first material on the research of runoff formation processes date from 1964. The goal of its creation was to establish relationships between runoff and its genetic and conditional factors, to design rainfall-runoff mathematical models, to quantify the way different topo-graphical and cultivated surfaces participate in the flow processes and to study the water balance in the soil.

The VEB is situated at an altitude of 500 m a.s.l. (45°05’07.27”N latitude and 25°15’15.43”E longitude) and it is located in the western extremity of the Curvature Sub-carpathians, on the left bank of Dâmboviţa River (Figure 1). The climate is moderate temperate-continental and the area of the VEB was characterized in the 1980-2014 period by an average multiannual rainfall depth of 806 mm. Most rainfalls occurred in the growing semester (63%), and the highest number of rainfalls events was recorded in June (12.6%) and July (12.4%). The lowest amount of precipitation was registered in the cold semester (October-March), with the lowest precipitations measured in January (5.21%) and February (5.7%). The average air temperature was 9.7°C and July was the month of the maximum temperature, with an absolute maximum of 37.3°C in 2000 (a dry year), while January is the month having the minimum temperatures (-22.6°C in 1979).

3.4 Experimental plots

Hydrological monitoring and field experiments at the micro-scale are aimed at:

  1. determining parameters of the water balance equation, during natural and simulated rainfall;

  2. research of runoff generation and soil erosion processes;

  3. transfer relation of runoff coefficients from a small scale to medium scale.

Experimental plots are of two types: water balance plots and runoff plots. The observations made during natural and simulated rainfall events included rainfall quantities, water depth, water turbidity, soil temperature, and soil moisture content.

The plots area is bordered with concrete walls, collection channels composed of gutters, underground pipes, and at their lower part there are shelters containing calibration tanks with drainage installation for evacuated of collected water.

Flow rates on plots are measured with the mechanic limnigraph (water level recorded) and automatic device, such as: pressure sensor and float-operated shaft encoder water level sensor. Automatic and continuous recordings of the water level drained from the plots into calibration tanks is done by means of a limnigraph (Valdai model), with daily change diagrams (limnigrama) at AEB and VEB, pressure sensors (U20L-04 model; accuracy: ±0.1% FS; from Onset HOBO) at AEB and float-operated shaft encoder water level sensors (OTT SE 200 model; accuracy: ±0.1% FS; from OTT) at VEB, which permits the recording of any change (volumetric method and variation in spillway) of the water depth collected in the tank (that has a full capacity of 0.46 m3). The limnigraphs and float-operated shaft encoder water level sensors, record the variation in water depth both inside the tank with the help of a floater and the water depth at the spillway; tanks have a spill-way with an opening at 45°. The water discharge calculation is done through the partial volumetric method – V (through division), the relationship beingV =f (H); also, water depth measurements are conducted with the help of pressure sensors.

Water turbidity (ρ) measurement is done through the “filtering method”; the procedure consists of collecting water samples (500 ml) from tanks – for runoff plots, filtering and drying them in the oven, followed by the calculation of associated sediment losses, after one flow.

The experimental plots from AEB are runoff plots. These have:

  1. an area of 80 m2 (20×4 m); 5.6% slope; W-E orientation; one of them is covered with perennial grass ”grassland” (RP1), while the other ”bare soil” (RP2) is devoid of grass through hoeing and the structure of the first soil horizon measuring 20 cm is modified from that of the first runoff plots, which led to a higher degree of infiltration compared to the first one (Figure 2 A,B);

  2. a portable rainfall simulator, used for the studies concerning overland flow; this tool generates artificial rains from nozzles (ø = 1 mm), with a controlled depth, intensity and duration; the structure consists of a 2 pipe section (ø = 37 mm) from metal (length = 20 m);

  3. three tipping bucket rain gauges (RG3-M, Onset HOBO data logger); bulk precipitation collectors (surface area ∼200 cm2; resolution: 0.2 mm; accuracy: ±1.0% FS); two of them are located at ground level and one at the height of 1.50 m (Figure 2A,B);

  4. four capacitance sensors (EC-5 model, accuracy: ± 1-2%) to measure electrical propriety of the soil (the dielectric permittivity -𝜀) and estimation the volumetric soil water (𝜃); set in the center of the plot at the depth of 10, 20, 40 and 60 cm and 1 rugged temperature sensor (at 10 cm depth), connected to the Em5b data logger from Decagon Devices Inc.

The experimental plots of VES are:

  1. water balance plots – for overland flow, subsurface flow and base flow monitoring have the following characteristics: eutricambisol – a type of soil with “28% clay, 21% silt, 51% sand” [23]; slope of 13% and N-S orientation (Table 1, Figure 3 A,B); between the plots there is one tipping bucket rainfall collector (RG3-M); six capacitance sensors (10HS model, accuracy: ± 1-2%); set in the center of the ”grassland” plot at the depth of 5, 40, 60, 80, 100 and 120 cm connected to the Em5b data logger from Decagon Devices Inc.

  2. runoff plots – for overland flow monitoring, have similar physiographic conditions with the first category of plots, with the single remark that they have different land uses; next to the plots, there are two pluviometers (Table 1).

Table 1

Characteristics of experimental plots within NIHWM.

Type of plotExperimental BasinDimension A/L*lNumber of plotLand use
water balance plotsVES300/30×101grassland
1bare soil
runoff plots10/5*21impermeable
20/10*21
40/20*21
40/10*41grassland
1bare soil
600/60*101grassland
900/90*101intensive apple orchards
900/90*101super intensive apple orchards
AEB80/20*41grassland
1bare soil

VES = Voineşti Experimental Basin; AEB = Aldeni Experimental Basin; A=area in m2; L=length and l = width in m

3.5 Hydrological monitoring and data acquisition

The observation and measurement program at AEB is carried out following the instructions and standard guidance of the NIHWM, e.g.A guide for the activity in the representative and experimental basins, Volume IV [24]. The instructions and guidebooks are made in accordance with the recommendations of Toebes & Ouryvaev [5], Technical regulations, Volume III[1] and Guide to Hydrological Practices, Volume I[2]. According to WMO (2006), this falls in the “hydrological stations for specific purposes” category, and the observation program is typical for a hydrometric station and for ”climatological and precipitation stations for hydro-logical purposes”.

The current modernization of the observation, collection and recording process of the elements necessary for a quantitative estimation of the water balance equation involves the upgrade and replacement of outdated equipment and instruments with modern equipment’s, devices and sensors. The measurements of the hydro-meteorological elements in automatic system, using the sensors, are nowadays used to compare the results with those from the classical systems for instruments’ calibration.

The modernization process focused on the development of data acquisition storage, data transfer (every 10 minutes); terminal emulation, numeric output and export functions. Transmission of hydrometeorological data is conducted through the Global System for Mobile Communications (GSM) to the NIHWM server or is downloaded from a data logger directly on a portable PC. Data transmitted through GSM from AEB are consulted for the required time interval (time taken and finish time) and can be viewed online in tabular format (such as: browser grid/data table/plain/fancy; spreadsheet .xls/zip) and downloaded.

3.6 Data processing, quality control and storage

Periodically (at the end of each month and year), after data collection – usually checked by a Hydrological Technician or Hydrologist – in printed paper and electronic format, the data are used for the hydrologic process of verification and expertise (data quality control). Afterwards, following positive solutions (validations), the data are stored in the database.

Hydrological data are used to better knowledge our water resources and disseminated through: relations updates (e.g. rainfall-runoff) (Figure 4); multiple correlations to reflect the role of various factors, research themes/projects; yearbooks of basic data (Experimental Basins Yearbook) and scientific papers.

4 Conclusions and perspectives

Experimental investigation in NIHWM is performed with experimental plots (water balance and runoff plots). The AEB and VES represent research units equipped with hydrometric instruments, designed for the experimental hydrological studies. Hydrological monitoring is currently undergoing a process of modernization due to the availability of new tools based on sensor and electronic data transfer technologies. The valorization of data acquired allows studies to be carried at micro-scale concerning the determination of the elements that make up the equation for hydric/water balance, in order to expand the application of the relation between runoff coefficients from a small scale to a medium scale. The future plans involve implementing research projects on subjects related to rainfall, runoff and sediment transport modeling, in order to substantiate the relationship between drainage and genetic and conditional factors.

Figure 2 The runoff plots (RP) of Aldeni Experimental Basins, in left “bare soil” plot -RP2 (A) and in right ”grassland” plot – RP1(B)
Figure 2

The runoff plots (RP) of Aldeni Experimental Basins, in left “bare soil” plot -RP2 (A) and in right ”grassland” plot – RP1(B)

Figure 3 The water balance plots “bare soil” (A) and shelter house equipped with calibrated tanks, limnigraph and water level sensor (B), from Voineşti Experimental Basin.
Figure 3

The water balance plots “bare soil” (A) and shelter house equipped with calibrated tanks, limnigraph and water level sensor (B), from Voineşti Experimental Basin.

Figure 3 Hydrographs of overland flow on runoff plots (RP) from natural – RP1 and RP2 (A) and artificial – RP1 (B) rainfall from Aldeni Experimental Basin.
Figure 3

Hydrographs of overland flow on runoff plots (RP) from natural – RP1 and RP2 (A) and artificial – RP1 (B) rainfall from Aldeni Experimental Basin.

Acknowledgement

The authors would like to thank the NIHWM, for allowing Ms. Gabriela MOROfiANU, currently studying for a master’s degree at the Faculty of Geography, University of Bucharest, to carry out practical activities, focused on documentation and research, in the team of the Section of Experimental Hydrology of NIHWM and for offering her the opportunity to use the facilities of the Aldeni Experimental Basin. Also, we thank two anonymous reviewers for their suggestions and comments which greatly improved the manuscript.

References

[1] Hopmans J.W., Pasternack G., Experimental hydrology: A bright future. Adv. Water Resour. , 2006, 29(2), 117-120.10.1016/j.advwatres.2005.04.016Search in Google Scholar

[2] Linsley R.K., Representative and experimental basins where next. Hydrol. Sci. Bull. , 2009, 21:4, 517-529.10.1080/02626667609491671Search in Google Scholar

[3] Ferreira Moreira L.F., de Oliveira Silva F., Chen S., de Almeida Andrade H.T., Tavares da Silva J.H., Marozzi Righetto A., Plot-Scale Experimental Studies. Soil Eros Stud., 2011, 7, 151-166.10.5772/23679Search in Google Scholar

[4] Lvovich M.I., Experimental soil-hydrologic water-balance investigations. International Association of Hydrogeologists, IAHS, FAO, 1965, 148(62), 1-12.Search in Google Scholar

[5] Toebes C., Ouryvaev V., Representative and experimental basins. An international guide for research and practice, A contribution to the International Hydrological Decade, United Nations Educational, Scientific and Cultural Organization, Paris, 1970.Search in Google Scholar

[6] Garcia G., Hickey W.C., Dortignac E.J., An inexpensive runoff plot (Vol. 12). Rocky Mountain Forest and Range Experiment Station, Forest Service, US Dept. of Agriculture, 1963.Search in Google Scholar

[7] Becker A., Nemec, J., Macroscale hydrologic models in support to climate research. The Influence of Climate Change and Climatic Variability on the Hydrologie Regime and Water Resources, 1987, 431-445.Search in Google Scholar

[8] Hudson N.W., Field measurement of soil erosion and runoff. FAO Soils Bulentin, Roma, 1993, 68, 140.Search in Google Scholar

[9] Schumann S., Schmalz B., Meesenburg H., Schröder U., Status and Perspectives of Hydrology in Small Basins. Results of the International Workshop in Goslar-Hahnenklee, 2009 and Inventory of Small Hydrological Research Basins, IHP/HWRP Berichte 10, Koblenz, 2010.Search in Google Scholar

[10] Mustaţă L., First results from the experimental hydrological stations and representative basins Studii şi cercetări, Hidrologie, XLIX, Institutul de Meteorologie şi Hidrologie, Bucureşti, 1980. (in Romanian)Search in Google Scholar

[11] Miţă P., Representative Basins in Romania, National Institute of Meteorology and Hydrology, Bucharest, 1996.Search in Google Scholar

[12] Blidaru S., First results on the formation of runoff from rain from the work conducted at Voineşti Experimental Hydrological station, Hydrological studies, XXVIII, Extras, Institutul de Meteorologie şi Hidrologie, Bucureşti, 1970. (in Romanian)Search in Google Scholar

[13] Diaconu C., Crăciun S., Results obtained in the study of runoff formation using radioactive tracers. Hydrological studies, XXXV, Institutul de Meteorologie şi Hidrologie, Bucureşti, 1973. (in Romanian)<a id=”page_”></a>Search in Google Scholar

[14] Petrescu M., Establishing relation between rain-infiltration, runoff, and suspended sediment load on low-slope surfaces, Studii de hidrologie, XLII (Extras). Institutul de Meteorologie şi Hidrologie. Bucuresti, 1974. (in Romanian)Search in Google Scholar

[15] Blidaru S., Drăgoi E., Stanciu P., Mathematical modelling of overland runoff under various physiographical conditions and for certain agricultural uses. The influence of man on the hydrological regime with special reference to representative and experimental basins. Proceedings of the Helsinki Symposium, IAHS-AISH, 1980, 130, 427-432.Search in Google Scholar

[16] Stanciu P., Zlate I., Mathematical modeling of discharge processes in experimental and representative watersheds. Studii şi cercetări, Hidrologie 2, Institutul de Meteorologie şi Hidrologie, Bucureşti, 1988, 17-32. (in Romanian)Search in Google Scholar

[17] Zlate I., Distributed runoff modelling in small catchment. Catchment hydrological and biochemical processes in the changing environment Seventh Conference of the European Network of Experimental and Representative Basins (ERB) Liblice (Czech Republic), 22 – 24 September 1998, UNESCO, Paris, 2000, 289-296.Search in Google Scholar

[18] Stanciu P., The water movement on permeable slopes. Publisher HGA, Bucureşti, 2002. (in Romanian)Search in Google Scholar

[19] Mociorniţă C., Birtu E., Some aspects regarding the suspended sediment load in Romania. Hidrotehnica, 1987, 32(7), 241-245. (in Romanian)Search in Google Scholar

[20] Zaharia L., Grecu F., Ioana-Toroimac G., Neculau G., Sediment transport and river channel dynamics in Romania – variability and control factors. In: Manning A. (Ed.), Sediment Transport in Aquatic Environments, Rijeka, Croatia, 2011, 293-316.10.5772/21416Search in Google Scholar

[21] Radu A., Muşat M., Parvan L., Urzică C., Sevastel M. Assessment, by soil survey, of condition of soil fertility and identification of its natural and human limiting factors in the CernăteştiManasia interbasinal area, Buzău county. Annals of the University of Craiova-Agriculture, Montanology, Cadastre Series, 2010, 40(1), 547-552.Search in Google Scholar

[22] Mutchler C. K., Runoff plot design and installation for soil erosion studies. ARS 41-79, Agricultural Research Service, U.S. Department of Agriculture, National Agricultural Library, Washington DC, 1963.Search in Google Scholar

[23] Maftei C., Chevalier P., Ciurea, C., Considerations Concerning the Characteristics of Permeability of the Podzolic Solil in Voinesti Catchment. Analele Universităţii “OVIDIUS” Constanţa, Seria Construcţii, 2002, I (3,4), 525-530.Search in Google Scholar

[24] Adler M-J., Minea G., Guide for the activity of the representative and experimental basins. Vol. IV. Institutul Naţional de Hidrologie şi Gospodărire a Apelor, Cuvinte cu minte, Bucureşti, 2014.Search in Google Scholar

Received: 2014-9-30
Accepted: 2015-10-23
Published Online: 2016-2-29
Published in Print: 2016-2-1

© 2016 G. Minea and G. Moroşanu, published by De Gruyter Open.

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

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