Ts. Mirtskhulava Water Management Institute of Georgian Technical University THE FIELD STUDY OF THE COMBINE THREE TIER DRAINAGE Givi Gavardashvili Director.

Slides:



Advertisements
Similar presentations
1 Water discharge rate is monitored continually. 2 Sampling of stream and drainage water is made automatically or by grab sampling weekly while groundwater.
Advertisements

S A L T M O D A computer program for the prediction of the salinity of soil moisture, ground water and drainage water, the depth of the water table, and.
1 Agricultural Research, Extension and Training Project ENVIRONMENT POLLUTION CONTROL PROGRAM Environment Friendly Agricultural Practices Ioseb Murvanıdze.Technıcal.
Workshop on Climatic Analysis and Mapping for Agriculture
Getahun Wendmkun Adane March 13,2014 Groundwater Modeling and Optimization of Irrigation Water Use Efficiency to sustain Irrigation in Kobo Valley, Ethiopia.
 Soil compaction :  Compaction is the reduction in voids content due to air being forced out of the soil or dissolved in the soil water by mechanical.
1 Toshihiko Anzai 1* Katsuyuki Shimizu 2, Yoshinobu Kitamura 2, and Jumpei Kubota 3 1:The United Graduate School of Agricultural Sciences, Tottori University.
Temporal patterns of infiltration into a water repellent soil under field conditions Phil Ward, Margaret Roper, Ramona Jongepier and Shayne Micin April.
Dale T Littlejohn Senior Geologist. What is fate and transport in the vadose zone? Vadose Zone Hydrocarbon release from buried pipeline Aquifer Surface.
Field Hydrologic Cycle Chapter 6. Radiant energy drives it and a lot of water is moved about annually.
R AINFALL -R UNOFF M ODELING O F W ADI Z IMAR. Prepared by Ahmad Tallal Abu-Hamed Mohamed Nemir Mohsen Osama Omar Nazzal Under the direction of Dr. Sameer.
Engineering Hydrology (ECIV 4323)
1 There are various techniques for estimating discharge for small watersheds. If you know the maximum discharge that you need to convey, how do you determine.
Drainage System Design and Layout. Design Process Flowchart Background Information (Soils, Topo, Crops) Confirm Outlet Drainage Needed Select DC, Spacing.
Lecture 3 Earthmoving Materials
INFLUENCES OF IRRIGATION AND N FERTILIZATION ON MAIZE (Zea mays L.) PROPERTIES - Hrvoje PLAVSIC1 - Marko JOSIPOVIC1 - Luka ANDRIC1 - Antun JAMBROVIC1 -
Surface Energy Budget Q*=Net radiation QE=Latent Heat Flux
HYDRUS_1D Sensitivity Analysis Limin Yang Department of Biological Engineering Sciences Washington State University.
Status report on Step1 of Task A, DECOVALEX-2011 modeling for Ventilation Experiment –modeling for Ventilation Experiment By Xiaoyan Liu, Chengyuan Zhang.
The Effect of Soil Hydraulic Properties and Deep Seepage Losses on Drainage Flow using DRAINMOD Debjani Deb 26 th April, 2004.
Universal college engineering & technology
Water in Soil. The basis of irrigation Soil Plant Evapotranspiration Plant requirements.
Lecture (3). Mechanical Analysis of Soil is the determination of the size range of soil particles, expressed as a percentage of total dry weight. The.
Construction Dewatering
Lecture (4).
Course No: CE 4000 INVESTIGATION ON THE PERFORMANCE OF BAMBOO REINFORCED CONCRETE BEAMS Supervised By: MUHAMMAD HARUNUR RASHID Presented By: MOHAMMAD TAREQ.
rd International Commission on Irrigation and Drainage, Executive Council Meeting, 7 th Asian Regional Conference And Irrigation Australia 2012.
MER Design of Thermal Fluid Systems Pumps and Fans Professor Anderson Spring Term
Sewer Hydraulics Gravity flow: full flow Gravity flow: Partial flow
Soil Water.
Future Research Develop a conceptual model which will measure the impact of the potential solutions on the watershed and the surrounding environment Determine.
Role Of Catchment Drain For Earth Slope Stability
STUDY OF THE ROUGHNESS CHARACTERISTICS OF PLANT SPECIES IN CALIFORNIA RIVERS By U.C.Davis J.Amorocho Hydraulics Laboratory.
Rapid assessment of seasonal in-field water management on micro irrigated annual and perennial crops in Central Italy. Graziano Ghinassi and Stefano Cecchi.
Arctic Temperatization Arctic Temperatization : A Preliminary Study of Future Climate Impacts on Agricultural Opportunities in the Pan-Arctic Drainage.
Presented by: 1. A measure of how easily a fluid (e.g., water) can pass through a porous medium (e.g., soils) 2 Loose soil - easy to flow - high permeability.
The influence of extreme meteorological phenomena on soil water regime of lowlands Institute of Hydrology - Slovak Academy of Sciences Bratislava, Slovak.
CARBON SEQUESTRATION BY HYBRID POPLARS IN THE PACIFIC NORTHWEST Dr. Jon D. Johnson Hybrid Poplar Research Program Washington State University - Puyallup.
Winter Processes in WEPS Fred Fox Wind Erosion Research Unit Manhattan, KS.
College of Engineering Civil Engineering Department
EVALUATION OF THE OPTIMUM NITROGEN FERTILIZER DEPENDING ON THE NITRATE CONTENT OF THE SOIL IN SWEET CORN PLANTATION I. Buzás - E. Hoyk - I. Cserni – Borsné.
RESULTS OF RESEARCH RELATED TO CHARIS IN KAZAKHSTAN I. Severskiy, L. Kogutenko.
Printed by Introduction: The nature of surface-atmosphere interactions are affected by the land surface conditions. Lakes (open water.
1. Measuring Soil Quality Soil quality integrates the physical, chemical, and biological components of soil and their interactions. Therefore, to capture.
DRAINMOD APPLICATION ABE 527 Computer Models in Environmental and Natural Resources.
Mixture of Saline and Non-Saline Irrigation Water Influences Growth and Yield of Lettuce Cultivars under Greenhouse Conditions A. A. Alsadon, M. A. Wahb-allah,
Improving of Household Sample Surveys Data Quality on Base of Statistical Matching Approaches Ganna Tereshchenko Institute for Demography and Social Research,
There are various techniques for estimating discharge for small watersheds. If you know the maximum discharge that you need to convey, how do you determine.
ONE-DIMENSIONAL ANALYSIS ON BEDEVOLUTION ACCOMPANING BANK EROSION Satoru Nakanishi Hokkaido University Graduate School Kazuyoshi Hasegawa Hokkaido University.
1 INTRODUCTION TO “Stratigrafia” The code in the workbook “stratigrafia” computes - longitudinal profiles; - water surface elevation; - sediment transport.
Agronomic Spatial Variability and Resolution What is it? How do we describe it? What does it imply for precision management?
N.L Mufute , LWRM, MSU / PRELIMINARY DESIGN STEPS AND SPRINKLER SELECTION –EXAMPLE ON PERIODIC-MOVE SYSTEMS N.L.
6. Drainage basins and runoff mechanisms Drainage basins Drainage basins The vegetation factor The vegetation factor Sources of runoff Sources of runoff.
1 Effects of Seasonality upon Water and Solute Movement in The Unsaturated Zone Sleem Kreba and Charles Maule Department of Agricultural and Bioresource.
Subsurface Drainage (Tile) Design Thomas F. Scherer NDSU Extension Agricultural Engineer (701)
STUBBLE BURNING AND TILLAGE EFFECTS ON SOIL ORGANIC C, TOTAL N AND AGGREGATION IN NORTHEASTERN SASKATCHEWAN S. S. Malhi 1 and H. R. Kutcher 1 1 Agriculture.
Filtration Processes Introduction
Sanitary Engineering Lecture 4
26 May, 2016 Panevėžys, Lithuania
Sanitary Engineering Lecture 7
TS. MIRTSKHULAVA WATER MANAGEMENT INSTITUTE OF GEORGIAN TECHNICAL UNIVERSITY ИНСТИТУТ ВОДНОГО ХОЗЯЙСТВА ИМЕНИ Ц. МИРЦХУЛАВА ГРУЗИНСКОГО ТЕХНИЧЕСКОГО УНИВЕРСИТЕТА.
Soil wetting patterns under porous clay pipe subsurface irrigation A. A. Siyal 1 and T. H. Skaggs 2 1 Sindh Agriculture University, Tandojam, Sindh, Pakistan.
S. P. Mazumdar, D. K.Kundu*, A. R.Saha and Debjani Ghosh Crop Production Division ICAR-Central Research Institute of Jute and Allied Fibres, Barrackpore,
Wood ash, the residue remaining from the combustion of bark, sawdust and yard waste for energy generation for forestry product operations, is an effective.
Кnun=(Lmax-Lmin)/Lmed (1)
The Institute of Hydrology of the Slovak Academy of Sciences,
Faith Simitz and Benjamin D. Duval
Agriculture University in Kraków Department of Water Engineering
Grain Size Analysis Sieve Analysis
Presentation transcript:

Ts. Mirtskhulava Water Management Institute of Georgian Technical University THE FIELD STUDY OF THE COMBINE THREE TIER DRAINAGE Givi Gavardashvili Director of Institute, Doctor of Technical Sciences, Professor Maka Guguchia Ph Student Panevezys, Lithuania 2016

INTRODUCTION On the background on the climate change, aiming at efficiently cultivating the wet agricultural plots of field (with the area of ha) on Kolkheti Valley, Georgia (the maximum average annual amount of precipitations varies between 2100 and 2300 mm), an option of installing a field stand to study a Combine Three Tier Drainage (Georgian Patent Certificate No. GE P 2005, 3573 В) is considered [1,2].

2. IDENTIFYING THE DISTANCE BETWEEN THE DRAINS A design model given in Figure 1 was used for hydraulic calculations of the Combine Three Tier Drainage. Fig. 1. Design model of a Combine Three Tier Drainage

Where is the drainage length, is the proportionality factor, the same as the filtration coefficient (cm/sec); - is the depth of drainage installation (m) and is the form coefficient of the elliptic nod of the Combine Three Tier Drainage, which depends on the radius of curvature of the elliptic nod of the three tier perforated drainage (m). By knowing the ground water depth, as well as soil, hydrogeological and climatic conditions, the air and water regime of the agricultural crops can be regulated by using the Combine Three Tier Drainage. Figure 2 shows the design model to identify the distance between the drains. (l/sec) (1)

Figure 2 shows the design model to identify the distance between the drains. Fig. 2. Design model to identify the distance between the drains Let us simplify expression (1): We identify the distance between the drains (b) as follows: if the agricultural plots of field are cultivated by installing the Combine Three Tier Drainage system, then the distance between the drains is calculated with formula (3), but when it is necessary to install a combined drainage in the areas occupied by perennial plantations, the drainage system is installed in the middle of interrow, between the rows of perennial plantations. By means of calculations, it is also possible to install the drainage system with more than one drainage line in the interrow of the rows of perennial plantations[3]. (2) (3) (m)

3. FIELD STUDY OF THE COMBINE THREE TIER DRAINAGE Aiming at conducting the field experiments of the Combine Three Tier Drainage, a study polygon was organized on the experimental base of the Agrarian College of Georgian Technical University in village Didi Jikhaishi, Samtredia Region (See Fig. 3). Fig. 3. Field polygon in village Didi Jikhaishi

During the trench excavation, different layers of ground were identified, which were sampled and studied at the laboratory. The relevant graphs are given in Figure 4, and the average diameters are calculated with the following expression: Fig. 4. Grain-size curve – (21) soil depth – 0,30 m. (20) – soil depth – 0,50 m. (19) – soil depth – 1,0 m.

Let us calculate the mean diameter ( ) for each sample with the following formula: Where is the weight indicator of each fraction in the ground mass, and is the diameter of the sieves (mm). (4) Soil depth – 0,30 m. Soil depth – 0,50 m Soil depth – 1,0 m.

Figure 5 shows the full technological cycle to design the model of the Combine Three Tier Drainage.

During operation of the drainage system

Based on the field studies, the water intake capacity of the Combine Three Tier Drainage from the agricultural plots was calculated. Figures 6 and 7 show the graphs of the water discharge transported from the first and second drainage pipelines. Q 1 (l /sec) t 1 (sec) Fig. 5. Graph of dependence Q 1 = f(t 1 ) for the first drainage pipe Q 1 (l /sec) t 1 (sec) Fig. 6. Graph of dependence Q 2 = f(t 2 ) for the second drainage pipe

3. CONCLUSIONS Aiming at reaching efficient drying of wetlands on Kolkheti Valley, a new structure of the Combine Three Tier Drainage was developed. 2. The theoretical studies were used to fix the proper distance between the drains of the Combine Three Tier Drainage system. Based in the gained theoretical values, a field stand of a Combine Three Tier Drainage was installed in village Didi Jikhaishi, Samtredia Region, west Georgia. An integral curve of the grain size of the soil and ground fractions sampled from the field polygon is gained at the laboratory, and consequently, the mean diameter of the soil and ground is calculated. The water conductivity effect of two drains of the Combine Three Tier Drainage system is identified through the field studies.

Thank you for attention