Water Requirements for Main Crops Grown Under Three Different Agro Ecological Zones, Zimbabwe

Similar documents
Crop Water Requirement. Presented by: Felix Jaria:

Development of Decision Support System for On-Farm Irrigation Water Management

CHAPTER 6: Irrigation scheduling

IRRIGATION SCHEDULING OF ALFALFA USING EVAPOTRANSPIRATION. Richard L. Snyder and Khaled M. Bali 1 ABSTRACT

OPTIMAL CROP WATER REQUIREMENT FOR ARANIAR RESERVOIR BASIN

Crop water requirements for tomato, common bean and chick pea in Hudeiba, River Nile State, Sudan

Crop Water Requirement Estimation by using CROPWAT Model: A Case Study of Halali Dam Command Area, Vidisha District, Madhya Pradesh, India

Evaluating the Consumptive Water Use of Teff in Consideration of Soil Water Movement in Central Ethiopia

Water Requirements and Irrigation Scheduling of Maize Crop using CROPWAT Model

Changes in crop evapotranspiration and irrigation water requirements

Agricultural Production Forecasting Using Planning Distribution Model (PDM):A Case Study of the Nam Oon Project

Determination of water requirement and irrigation timing for Amaranthus hybridus in Maiduguri metropolis, north-eastern Nigeria

A Computer program for Calculating Crop Water Requirements

Crop Water Requirements and Irrigation Scheduling

APPLICATIONS OF AN OPERATIONAL COMPUTER PROGRAM FOR IRRIGATION PLANNING AND MANAGEMENT IN ROMANIA

Assesment of Crop and Irrigation Water Requirements for Some Selected Crops in Northwestern Bangladesh

Water balance of savannah woodlands: a modelling study of the Sudanese gum belt region

5.5 Improving Water Use Efficiency of Irrigated Crops in the North China Plain Measurements and Modelling

Estimation of Irrigation Water Requirement of Maize (Zea-mays) using Pan Evaporation Method in Maiduguri, Northeastern Nigeria

Michael Cahn and Barry Farrara, UC Cooperative Extension, Monterey Tom Bottoms and Tim Hartz, UC Davis

Water Footprint Evaluation of Oryza sativa L.Tha Wang Pha District, Nan Province

Monitoring soil moisture helps refine irrigation management

Effect of Deficit Irrigation on Growth and Yield of Sugarcane

DETERMINATION OF CROP CO-EFFICIENT AND CROP WATER REQUIREMENT OF MUNGBEAN ( VIGNA RADITA L. ) IN DL1B AGRO ECOLOGICAL REGION OF SRI LANKA

Nutrition of Horticultural Crops Measurements for Irrigation. Lincoln Zotarelli Horticultural Sciences Department University of Florida Spring 2015

Estimation of irrigation water requirement of maize (Zea-mays) using pan evaporation method in maiduguri, Northeastern Nigeria

Drip irrigation scheduling

Cristian Paltineanu 1, Emil Chitu 2 and Emilia Mateescu 3

Water requirements for major crops in different agro-climatic zones of Iraqi Kurdistan using by CROPWAT 8.0

REFERENCE EVAPOTRANSPIRATION ESTIMATION USING CROPWAT MODEL AT LUDHIANA DISTRICT (PUNJAB) A. Patel 1, R. Sharda 2, S. Patel 3 and P.

Figure 1: Schematic of water fluxes and various hydrologic components in the vadose zone (Šimůnek and van Genuchten, 2006).

Crop Water Requirement using Single and Dual Crop Coefficient Approach

GSJ: Volume 6, Issue 4, APRIL GSJ: Volume 6, Issue 4, April 2018, Online: ISSN

ANALYSIS OF RAINFALL DATA TO ESTIMATE RAIN CONTRIBUTION TOWARDS CROP WATER REQUIREMENT USING CROPWAT MODEL

Determination of the Optimal Date for Sowing of Wheat in Canal Irrigated Areas using FAO CROPWAT Model

Lecture 5: Transpiration

Statistical Comparison of Reference Evapotranspiration Methods: A Case Study from Srinagar in J&K, India

M= Rank No. N= no. of years

Studying effects of different irrigation levels and planting patterns on yield and water use efficiency in potato (Solanum tuberosum L.

REFERENCE EVAPOTRANSPIRATION: CHOICE OF METHOD

ITALIAN AGRICULTURAL PRODUCTION AND THE HEAT WAVE DURING SUMMER Luigi Perini 1 and M. Carmen Beltrano Ministry of Agriculture, Rome, Italy

A NEW TECHNIQUE FOR EVALUATION OF CROP COEFFICIENTS:A CASE STUDY

Crop water requirement and availability in the Lower Chenab Canal System in Pakistan

Evaluate the Effect of Low Cost Drip Irrigation on the Yield and Production Efficiency of Onion Crops

Evaluation of the Efficiency of CROPWAT Model for Determining Plant Water Requirement in Arid Regions

Managing fertilization and irrigation for water quality protection

Fecha 17/octubre/2018

Optimizing irrigation requirements for almond trees grown in the South Sinai Governorate

08. WATER BUDGETING AND ITS IMPORTANCE - IRRIGATION SCHEDULING - APPROACHES

Water Management: A Complex Balancing Act

Water requirement of wheat crop for optimum production using CROPWAT model

ESTIMATION OF EVAPOTRANSPIRATION AND CROP WATER REQUIREMENTS OF SOME SELECTED CROPS AT TONO IRRIGATION SCHEME IN THE UPPER EAST REGION OF GHANA

FORECASTING CROP WATER REQUIREMENT BY ET-HS MODEL FOR ARID AND SEMI ARID REGION OF IRAN

ORCHARD GROUNDCOVER MANAGEMENT: LONG-TERM IMPACTS ON FRUIT TREES, SOIL FERTILITY, AND WATER QUALITY

Assistant Professor, Civil Engineering Department Dr. D Y Patil Institute of Engineering Management and Research Akurdi, Pune (MH), INDIA

Drip Irrigation Efficiency. Fact or Fiction?

THE FAO PENMAN MONTIETH METHOD OF ESTIMATING EVAPOTRANSPIRATION COMPARED WITH NINE OTHER METHODS IN CAPE COAST MUNICIPALITY, GHANA

Crop Water Requirements. Lecture note for Soil and Water Management Course Prepared by Dr ND Nang

Comparison of water drainage and nitrate leaching under three land use types in the North China Plain

AquaCrop theoretical and practical training

The control head. The water pipelines. The dripper lines. IRRIGATION SCHEDULING Irrigation requirements

Effect of Irrigation System Basin and Furrow in Saline Distributions Patterns and Productivity Corn (Zea Mays L.)

Indian Journal of Hill Farming

Russia and Central Asian Countries

Prediction of Traditional Climatic Changes Effect on Pomegranate Trees Under Desert Condition in EL- Maghara, Egypt

Special Report Concerning Irrigation Scheme

Use of the FAO CROPWAT model in deficit irrigation studies

IV International Symposium Agrosym /AGSY S VIRTUAL WATER BALANCE ESTIMATION IN AN IRRIGATED AREA IN NORTH-EASTERN TUNISIA.

CLIMATE CHANGE AND THE HYDROTHERMAL AND EVAPOTRANSPIRATION CONDITIONS IN THE PLANNING REGIONS OF BULGARIA

Michael Cahn, Barry Farrara, Tim Hartz, Tom Bottoms, and Mark Bolda

Lecture 1: Importance of Irrigation and Drainage

The application of climatic data for planning and management of sustainable rainfed and irrigated crop production

Water Requirements of Qat (Catha edulis) Cultivation in the Central Highlands of Yemen

Effect of fertilizer strategies on the grey water footprint in rain-fed and irrigated agriculture

Effects of differential irrigation practices on yield of sugarcane at Kenana Sugar Scheme, Sudan

Study of applications of a modernized sprinkler irrigation system

Effects of the decoupling of the subsidies on agricultural water productivity

What s all the Fuss About ET Controllers? The Current State of Landscapes. Why the Need Public Agency Studies What s s Next.

Embankment and cut slope monitoring and analysis

Mapping irrigated areas and water consumption in Crete

WATER PRODUCTION FUNCTIONS FOR CENTRAL PLAINS CROPS

ESTIMATION OF EVAPOTRANSPIRATION IN SARDAR SAROVAR COMMAND AREA USING WEAP

Use of GIS and remote sensing in identifying recharge zones in an arid catchment: a case study of Roxo River basin, Portugal

Lecture 19. Landfill hydrology

Revised FAO Procedures for Calculating Evapotranspiration Irrigation and Drainage Paper No. 56 with Testing in Idaho 1

Management of Runoff Harvesting as a Source of Irrigation Water in Dry Land Agriculture on Steep Land Slope

Procedure to easily Fine-Tune Crop Coefficients for Irrigation Scheduling

Nicola Minerva - Beta ADVANCES IN SUGAR BEET IRRIGATION Valladolid 5 June

TheHelper, A User-Friendly Irrigation Scheduling Tool In Florida and Hawaii A. Fares 1, M. Zekri 2 and L.R. Parsons 2. Abstract

Estimation of Evapotranspiration using CROPWAT 8.0 Model for Shipra River Basin in Madhya Pradesh, India

Under drought conditions when water may be in short supply, growers often need to

Hamdy A. (ed.). Regional Action Programme (RAP): Water resources management and water saving in irrigated agriculture (WASIA PROJECT)

ET-BASED IRRIGATION SCHEDULING

ABSTRACT. KEYWORDS: Reference Evapo transpiration (ETo), Blaney-Criddle Method, Penman-Monteith Method, Irrigation NOMENCLATURE

Integrate GIS and Cropwat Model in Study Crop Water Requirement and Irrigation Scheduling

Lysimeter based water requirements and crop coefficient of surface drip-irrigated date palm in Saudi Arabia

Estimation irrigation water requirements with derived crop coefficients for upland and paddy crops in ChiaNan Irrigation Association, Taiwan

Evaluation of Deficit Irrigation Strategies for Corn

How to irrigate. How much to irrigate. When to irrigate

Analyzing water resources in a monsoon-driven environment an example from the Indian Western Ghats

Transcription:

Middle East Journal of Agriculture Research ISSN 277-465 Volume: 5 Issue : 1 Jan.-Mar. 216 Pages: 14-28 Water Requirements for Main Crops Grown Under Three Different Agro Ecological Zones, Zimbabwe 1 Gamal Abdel Rahman, 2 A. M. Talaat and 1 C. Zawe 1 Soil and Water Management, Irrigation Department, Zimbabwe. 2 Desert Research Center, Egypt. Received: 7 December 215 / Accepted: 25 December 215 / Publication date: 1 January 216 ABSTRACT The current work was carried out in the Agriculture Experimental Stations of, and Marondera in Zimbabwe, for studying the water requirements of some field crops; wheat, barley, maize, potatoes, sugar beet, cowpea, soybeans and sunflower grown in and regions and some vegetables crops, onion, cabbages, tomatoes, spinach, covo and Chinese cabbage, in Marondera region. The period of "heavy rains" reaches its maximum value in early December to February and the rain season starts from October to April every year in these regions. Effective rainfall attributed the water requirements during the entire growth cycle of maize, potatoes, sugar beet, cowpea, soybeans and sunflower in and regions, that irrigation is unnecessary in some months from December to February. Also the irrigation intervals (days) of crops vary from 5 to 25 during the growth seasons in all experimental stations. Data of water requirements and irrigation scheduling for seasonal crops grown in both stations, were predicted on the basis of climate, soil type and crop coefficients. The results showed that water requirements of summer crops were higher than those of winter crops for all experimental stations, except for maize. Also, the water requirements of winter crops and vegetables were higher than those of summer crops. Irrigation requirements decreased than water requirements by subtracting the contributions of effective rainfall. Using Sub-surface, drip, sprinkler, gated and siphon irrigation systems can respectively save up to 44%, 41%, 33%, 28% and 23% of water if compared to surface irrigation system. In Marondera, The water requirements for onion as compared to the climatic potential, also indicates water requirements during the growth cycle of onion from March to October under many irrigation systems. The analysis shows that in this region, the total seasonall quantities of water ranged between 8876 to 15977 m 3 /he/season. The daily needs ranged from 23.32 to 93.97 m 3 /hectare/day Key words: Water requirements, field crops, and regions, Zimbabwe. Introduction Water is one of the most precious and heavily scrutinized natural resources worldwide. Particularly in arid and semi-arid regions and improving agricultural water use efficiency is vitally important in parts of the world that have limited water resources. Innovative irrigation solutions must address the water scarcity problems affecting arid countries. Jensen et al. (199) defined irrigation water requirements as the quantity of water exclusive of precipitation that is required for various beneficial uses. The net irrigation requirements per unit area is the water that must be supplied by irrigation to satisfy ET, leaching and miscellaneous water requirements that are not provided by water stored in the soil and precipitation that enters the soil. Precipitation that drains through a soil is not effective unless it reduces the leaching requirement Allen et al. (1998) concluded that FAO Penman Monteith method is recommended as the sole method for determining ETo. The method has been selected because it closely approximates grass ETo as the location evaluated is physically based, and explicitly incorporates both physiological and aerodynamic parameters. The worldwide use of surface and subsurface drip irrigation systems has increased considerably in recent decades. The main advantage of this system is the potential to increase crop yields while reducing water application, fertilizer and cultivation costs. The soil moisture distribution pattern around a water emitter depends on: (i) the total volume of water applied; (ii) the emitter flow rate, source configuration (surface, subsurface, point or line) and initial boundary conditions; (iii) the soil physical properties and their spatial distribution; (iv) plant root activity ; and (v) irrigation management, El-Maloglou et al. (21) also identified that surface and subsurface drip irrigation system can increase water use efficiency but only if the system is designed to meet the soil and plant conditions. irrigation can achieve high water use efficiencies, but only when the system is designed correctly, with appropriate emitter spacing, flow rate and installation depth (Phene, 1995). Corresponding Author: Gamal Abdel Rahman, Soil and Water Management, Irrigation Department, Zimbabwe 14

The type of irrigation system is important and the availability of suitable irrigation systems meets the needs of agricultural expansion. Irrigation water is rapidly becoming the primary limiting factor for crop production. Surface and subsurface drip irrigation systems were proven to increase water productivity (Mailhol et al., 211). The soil moisture distribution patterns showed that the vertical movement of soil moisture was higher than the horizontal movement under both Surface and subsurface drip irrigation systems. The overall wetted area, delimited by the wetting front was largest for the manually controlled irrigation scheduling with both Surface and subsurface drip irrigation systems, the smallest for the smart controller irrigation scheduling under both Surface and subsurface drip irrigation systems, (Al-Ghobari and El-Marazky, 212) Materials and Methods Experimental Site: The study was conducted at, and Marondera Research Stations in Zimbabwe. Field crops: Season Crops Planting Date Harvesting Date Winter Wheat 1-May 3-Sep Barley 1-May 3-Sep Maize 14-Oct 3-Mar Potatoes 1-Aug 28-Dec Summer Sugar Beet 1-Feb 3-Jun Cowpea 1-Feb 21-May Soybeans 15-Nov 14-May Sunflower 15-Nov 14-May Winter Onion 15-Mar 12-Oct Cabbages 15-May 13-Oct Tomatoes 15-Sep 12-Feb Summer Spinach 15-Aug 13-Jan Covo 15-Sep 12-Feb Chinese Cabbage 18-Oct 12-Mar Climatologic data: Potential evapotranspiration (ETo) m m / day: Meteorological data for the concerned regions were collected from the meteorological stations located at the experimental sites in, and Marondera to compute ETo rates using Penman Monteith equation as recommended by the FAO Expert Consultation held in May 199 in Rome, Italy, by using CROPWAT, software version 5.7 (Smith,1992). The amounts of applied irrigation water: D iw = (ETO*Kc) /Ea (Doorenbos and Pruitt, 1984) D iw = {((ETo*Kc) Pe)/(1-LR)}/Ea for field crops Where, D iw = Applied irrigation water, (mm) Kc = Crop coefficient LR = leaching requirements Ea = efficiency (%) Pe = Effective rainfall (mm) (((ETcrop*Kr)/Ea) (Pe mm))+lr Effective Rainfall (Pe): Pe =.8 P 25 (if P > 75 mm/month) Pe =.6 P 1 (if P < 75 mm/month) Brouwer et al. (1989). P = Rainfall (mm) Field irrigation schedules: I = ((p. Sa). D) / (ETc Pe) Doorenbos and Pruitt, (1984) Sa = (F.C.% - W.P. %) x d b x 1. Where: I = Interval of irrigation (days). P = Fraction of available soil water permitting unrestricted evapotranspiration. 15

Sa = total available soil water, mm/m soil depth. D = Rooting depth, (m) Etc = maximum crop evapotranspiration (mm) = ETo X Kc. Pe = effective rainfall (mm) F.C. = field capacity of soil water, %. W.P. = wilting point of soil water, %. d b = bulk density of soil, g / cm 3. Soil Properties: Determined for and Experimental Stations as following: and Marondera Soil Texture Sandy loam Sandy loam Sandy Clay Loam Sandy Clay Loam ph 5.8 6.5 EC soil (ds/m) 2.2 3.1 EC water (ds/m) 3.9 4.69 F.C (%) 2.33 2. W.P (%) 9.53 8.9 Bulk density g/cm3 1.5 1.55 AW. (mm) 162 172 Results and Discussion Climate: Meteorological data were collected from the meteorological station located inside the experimental fields at, and Marondera with altitude of about 1475 meter above sea level, latitude is 17 o 37` S. and longitude is 31 o 8` E. These data are presented in table (1) and Fig. (1). Table 1: Average mean of meteorological data of the studied areas at the Research Stations, Zimbabwe. Elements Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Avg. Maximum Temp C 26.7 26.4 26.6 25.7 24.1 22.1 21.9 24.4 27.8 28.9 28.5 27. 25.8 Minimum Temp C 16.1 15.8 15. 12.8 9.7 7. 6.7 8.9 12.3 14.6 15.8 16. 12.6 Relative Humidity (%) 78. 77. 75. 69. 65. 62. 6. 52. 46. 49. 58. 74. 63.8 Wind speed (km/hour) 14.4 14.4 14.76 14.4 12.6 13.32 17.64 18. 19.8 18.36 17.28 15.12 15.72 Sunshine (hr) 6.6 6.6 7.4 8.2 8.8 9.1 9.2 9.8 9.8 9.3 7.8 6.4 8.3 ETo (mm/day) 3.7 4.5 4.67 5.17 5.16 5.6 5.37 6.21 7.14 6.75 5.54 3.93 5.23 Total rain (mm/month) 19.8 176.3 99.1 37.2 7.4 1.8 2.3 2.9 6.5 4.4 93.2 182.7 84.6 9. 8. 7. 6. 5. 4. 3. 2. 1.. Maximum Temp C Minimum Temp C Relative Humidity (%) Mean wind speed (km/houre) Sunshine (hr) ETo (mm/day) Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec s Fig. 1: Average mean of meteorological data of the studied areas at the Research Stations, Zimbabwe. From table (1) the studied areas were characterized by high annual rainfall, about 84.6 mm / year and ranged between 1.8 to 19.8 mm/month. The rainfall occurs over a long period (October to April). The maximum air temperature ranges between 21.1 ºC (June) and 28.9 ºC (November), with an annual mean of 25.8 ºC, while the minimum air temperature ranges between 6.7 ºC (July) and 16.1 ºC (January), with an annual mean of 12.6 ºC. The Relative humidity is generally moderate and reaches 46 % in September and about 78 % in January, with an annual mean of 63.8 %. The sunshine hours ranges between 6.4 hours in December to 9.8 hours in August and September, with an annual mean of 8.3 hour. The wind velocity ranges between 12.6 16

km/hour in May and 19.1 km/hour in September, with an annual mean of 15.72 km/hour. In terms of the FAO Classification (Doorenbos and Pruitt, 1984), wind velocity at the areas under consideration could be described as moderate. This leads to the fact that such areas are subjected to physical erosion, mainly due to rainfall and wind action. The reference evapotranspiration, varies widely form 3.7 mm/day in January to 7.14 mm/day in September, with an annual mean of 5.23 mm/day. The mean annual is moderate (199 mm/year). Effective rainfall: Rainy season starts in October and finished in April (Table, 2) and (Fig., 2). The amounts of rain water varied between 1.8 and 19.8 mm/month with total of 84.6 mm/year. The amounts of effective rainfall water varied between 12.32 and 127.64 mm/month with a total of 495.24 mm/year. The quantities of water provided by effective rainfall vary between.41 and 4.14 mm / day, while Evapotranspiration needs for crops range between 3.7 and 7.14 mm/day from January to December, which corresponds to the period when all crops water requirements are greatest except wheat and barley. Similar results were obtained by Dastane, (1978) and Brouwer et al. (1989) Table 2: Rain and effective rainfall (mm/month) of the studied areas at Research Stations, Zimbabwe. Elements Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Avg. Total rain 19.8 176.3 99.1 37.2 7.4 1.8 2.3 2.9 6.5 4.4 93.2 182.7 84.6 Eff. rainfall 127.64 116.4 54.28 12.32 14.24 49.56 121.16 495.24 Eff. rainfall 4.12 4.14 1.75.41......46 1.65 3.91 1.37 25 Total rain (mm/month) Effective rainfall (mm/month) 2 (mm) 15 1 5 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec s Fig. 2: Rain and effective rainfall (mm) of the studied area at Research Station, Zimbabwe. Examination of the two curves (Fig. 3) shows that the rainfall exceeds superior the water requirements during the entire growth cycle of crops from December to February. This means that the water requirements for some crops are fully met by rainwater during this period, and that irrigation is unnecessary. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). Water requirements for wheat: Table (3) and Figure (4) illustrate the water requirements for wheat as compared to the climatic potential in and regions, Zimbabwe; they also indicate water requirements during the growth cycle of wheat from May to September under many irrigation systems. The analysis shows that in this region, the quantities of water ranged between 5499 to 9899 m3/he/season. The daily needs ranged from 17.22 to 123.51 m3/hectare/day. The lowest values are obtained in May, but the highest values obtained in July for many irrigation systems in both sites. The corresponding quantities of are almost the same. 17

The values range is in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation needs grow until the end of the growth cycle, as shown by the curve. Irrigation intervals ranged from 1 to 21 days during the growth season. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). (mm/day) 8. 7. 6. 5. 4. 3. 2. 1.. ETo (mm/day) Rainfall (mm/day) Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec s Fig. 3: Aridity factor of the studied area at Research Station, Zimbabwe. Table 3: Water requirements (m 3 /hectare/day) of wheat grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface May 18.2 17.22 2.66 22.14 23.84 3.99 18.2 17.2 2.64 22.12 23.82 3.97 Jun 44.6 42.13 5.55 54.16 58.33 75.83 44.6 42.7 5.49 54.9 58.26 75.73 Jul 72.7 68.61 82.34 88.22 95.1 123.51 72.6 68.55 82.26 88.13 94.91 123.39 Aug 51.1 48.28 57.94 62.8 66.85 86.91 51.1 48.27 57.92 62.6 66.83 86.88 Sep 33.6 31.72 38.7 4.79 43.92 57.1 33.6 31.74 38.9 4.81 43.95 57.13 m 3 /ha/season 5823 5499 6599 77 7614 9899 5818 5495 6594 765 768 9891 Water requirements of barley: Table (4) and Figure (4) show that the water requirements of barley grown in and regions, Zimbabwe; follow the same trend of wheat. The water requirements vary from May to September under many irrigation systems. The quantities of water ranged between 5475and 9856 m3/he/season. The daily needs ranged from 17.22 to 123.51 m3/hectare/day. The lowest values are obtained in May, but the highest values are obtained in July for many irrigation systems. The values ranges are in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation needs grow until the end of the growth cycle, as shown by the curve. Irrigation intervals ranged from 1 to 21 days during the growth season. Similar results were obtained by Robina et al. (27), Abdel-Rahman et al. (28)a,b and Abdel-Rahman et al. (21). Water requirements of maize: Table (5) and Figure (4) present the water requirements for maize in and regions, Zimbabwe. Effective rainfall (the amount of rainwater actually used by crops) increases from planting time to the end of April. During this period, the water requirements for maize, which range from 18.16 to 94.24 18

m 3 /hectare/day, are generally met. The quantities of water vary between 4841 to 8715 m 3 /he/season. Irrigation intervals ranged from 11 to 13 days during the growth season. The trend shows that water requirements for maize in this region are met particularly by the amount of rainwater which is available to crops. This tendency continues from October until March. Complementary irrigation is therefore needed to mitigate the water deficit. Irrigation needs grow until the end of the growth cycle, as shown by the curve. The lowest are values obtained in October, but the highest values are obtained in December for many irrigation systems for both sites. The values ranges are in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Similar results were found by Robina et al. (27), Abdel-Rahman et al. (28) a,b and Abdel-Rahman et al. (21). 16 Sub-surface Siphon Surface 14 12 1 (m 3 /hectar/season) 8 6 4 2 Wheat Barley Maize Potatoes Sugar Beet Cowpea SoyabeansSunflower Crops Fig. 4: Water requirements (m 3 /hectar/season) of crops grown in and regions, Zimbabwe. Table 4: Water requirements (m 3 /hectare/day) of barley grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface May 18.23 17.22 2.66 22.14 23.84 3.99 18.21 17.2 2.64 22.12 23.82 3.97 Jun 44.61 42.13 5.55 54.16 58.33 75.83 44.55 42.7 5.49 54.9 58.26 75.73 Jul 72.65 68.61 82.34 88.22 95.1 123.51 72.58 68.55 82.26 88.13 94.91 123.39 Aug 51.12 48.28 57.94 62.8 66.85 86.91 51.1 48.27 57.92 62.6 66.83 86.88 Sep 25.19 23.79 28.55 3.59 32.94 42.83 25.21 23.8 28.57 3.61 32.96 42.85 m 3 /ha/season 5797 5475 6571 74 7582 9856 5793 5471 6565 734 7575 9848 Table 5: Water requirements (m 3 /hectare/day) of maize grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface Nov. 58.7 55.44 66.53 71.29 76.77 99.8 58.9 55.62 66.74 71.51 77.1 1.12 Dec 32.3 3.54 36.65 39.27 42.29 54.98 32.5 3.7 36.84 39.47 42.5 55.25 Aug 32.9 31.4 37.25 39.91 42.98 55.87 32.9 31.3 37.23 39.89 42.96 55.85 Sep 67.2 63.44 76.13 81.57 87.85 114.2 67.2 63.48 76.18 81.62 87.9 114.27 Oct 88.9 83.99 1.79 17.99 116.3 151.19 89.1 84.14 1.97 18.19 116.51 151.46 m 3 /ha/season 8458 7988 9585 127 116 14378 8474 83 963 1289 1181 1445 Water requirements of potatoes: Table (6) and Figure (4) present the water requirements for potatoes grown in and regions, Zimbabwe. Effective rainfall (the amount of rainwater actually used by crops) increases from October to the end of December. During this period, the water requirements for potatoes, which range from 3.54 to 19

151.19 m 3 /hectare/day, are generally met. The quantities of water vary from 7988 to 14378 m 3 /he/season. Irrigation intervals ranged from 5 to 12 days during the growth season. The lowest values are obtained in December, but the highest values are obtained in October for many irrigation systems. The values ranges are in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems for both sites. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). Water requirements of Sugar Beet: Table (7) and Figure (4) present the water requirements for sugar beet in and regions, Zimbabwe. Effective rainfall increases from February to April. During this period, the water requirements of sugar beet, range from 15.75 to 124.14 m 3 /hectare/day. The quantities of water vary from 6675 to 1215 m 3 /he/season. Irrigation intervals ranged from 1 to 25 days during the growth season. The same results were obtained for site. The lowest values obtained in February, but the highest values obtained in April for many irrigation systems. The values are ranged in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Similar results were obtained by Robina et al. (27), Abdel-Rahman et al. (28)a,b and Abdel-Rahman et al. (21). Water requirements of cowpea: Table (8) and Figure (4) present the water requirements for cowpea in and regions, Zimbabwe. Effective rainfall increases from February to April. During this period, the water requirements of cowpea, which range from 18. to 18.62 m 3 /hectare/day. The quantities of water are varying between 463 to 7314 m 3 /he/season. The other site a little bit difference. The lowest values are obtained in February, but the highest values are those of April for many irrigation systems. The values are in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 1 to 23 days during the growth season. Similar results were reported by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). Table 6: Water requirements (m 3 /hectare/day) of potatoes grown in and regions, Zimbabwe. Subsurfac Siphon Surface e Siphon Surface Nov. 58.7 55.44 66.53 71.29 76.77 99.8 58.9 55.62 66.74 71.51 77.1 1.12 Dec 32.3 3.54 36.65 39.27 42.29 54.98 32.5 3.7 36.84 39.47 42.5 55.25 Aug 32.9 31.4 37.25 39.91 42.98 55.87 32.9 31.3 37.23 39.89 42.96 55.85 Sep 67.2 63.44 76.13 81.57 87.85 114.2 67.2 63.48 76.18 81.62 87.9 114.27 Oct 88.9 83.99 1.79 17.99 116.3 151.19 89.1 84.14 1.97 18.19 116.51 151.46 m 3 /ha/season 8458 7988 9585 127 116 14378 8474 83 963 1289 1181 1445 Table 7: Water requirements (m 3 /hectare/day) of sugar beet grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface Feb 16.7 15.75 18.9 2.25 21.81 28.36 16.7 15.81 18.98 2.33 21.9 28.47 Mar 41.2 38.92 46.7 5.4 53.89 7.5 41.3 39 46.8 5.14 54 7.2 Apr 73 68.97 82.76 88.67 95.49 124.14 73.1 68.99 82.79 88.7 95.53 124.19 May 6.8 57.39 68.86 73.78 79.46 13.3 6.7 57.34 68.81 73.73 79.4 13.22 Jun 41.6 39.32 47.18 5.55 54.44 7.78 41.6 39.27 47.12 5.49 54.37 7.68 m 3 /ha/season 768 6675 81 8582 9243 1215 77 6677 813 8585 9245 1219 Table 8: Water requirements (m 3 /hectare/day) of cowpea grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface Feb 19.1 18 21.6 23.15 24.93 32.41 19.1 18.7 21.69 23.24 25.3 32.53 Mar 41.2 38.92 46.7 5.4 53.89 7.5 41.3 39 46.8 5.14 54 7.2 Apr 63.9 6.34 72.41 77.59 83.56 18.62 63.9 6.37 72.44 77.61 83.59 18.66 May 27.3 25.82 3.99 33.2 35.76 46.48 27.3 25.8 3.96 33.18 35.73 46.45 m 3 /ha/season 432 463 4876 5224 5626 7314 437 468 4881 523 5633 7322 2

Water requirements of soybeans: Table (9) and Figure (4) present the water requirements for soybeans in and regions, Zimbabwe. Rainfall occurred from November to May. During this period, the water requirements of soybeans,which range from 22.95 to 89.12 m 3 /hectare/day. The quantities of water vary between 6436 to 11584 m 3 /ha/season. Water requirements of sunflower: Table (1) and Figure (4) present the water requirements for sunflower in and regions, Zimbabwe. Rainfall occurred from the plant date in November February to the end of growth in May. During this period, the water requirements of sunflower, range from 2.9 to 9.74 m 3 /hectare/day. The quantities of water vary between 7136 and 12845 m 3 /he/season. The lowest values are obtained in May, but the highest values are in February for many irrigation systems. The values ranged in are order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 1 to 25 days during the growth season. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27): Table 9: Water requirements (m 3 /hectare/day) of soybeans grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface Nov. 26.1 24.64 29.57 31.68 34.12 44.36 26.2 24.72 29.66 31.78 34.23 44.5 Dec 34.7 32.72 39.27 42.7 45.31 58.9 34.8 32.89 39.47 42.29 45.54 59.2 Jan 43.6 41.14 49.37 52.9 56.97 74.6 43.8 41.37 49.64 53.18 57.28 74.46 Feb 52.4 49.51 59.41 63.66 68.55 89.12 52.6 49.7 59.64 63.9 68.82 89.47 Mar 41.2 38.92 46.7 5.4 53.89 7.5 41.3 39 46.8 5.14 54 7.2 Apr 3.4 28.74 34.48 36.95 39.79 51.73 3.4 28.75 34.5 36.96 39.8 51.74 May 24.3 22.95 27.55 29.51 31.78 41.32 24.3 22.94 27.52 29.49 31.76 41.29 m 3 /ha/season 6814 6436 7723 8274 8911 11584 6837 6457 7748 832 894 11622 Table 1: Water requirements (m 3 /hectare/day) of sunflower grown in and regions, Zimbabwe. surface Sub- Siphon Surface Siphon Surface Nov. 22.8 21.56 25.87 27.72 29.86 38.81 22.9 21.63 25.96 27.81 29.95 38.93 Dec 34.7 32.72 39.27 42.7 45.31 58.9 34.8 32.89 39.47 42.29 45.54 59.2 Jan 46.6 44.2 52.83 56.6 6.95 79.24 46.9 44.26 53.11 56.91 61.29 79.67 Feb 53.4 5.41 6.49 64.81 69.8 9.74 53.6 5.61 6.73 65.7 7.7 91.9 Mar 49.5 46.7 56.4 6.4 64.66 84.6 49.6 46.8 56.16 6.17 64.8 84.24 Apr 45.6 43.1 51.72 55.42 59.68 77.59 45.7 43.12 51.74 55.44 59.7 77.62 May 21.3 2.9 24.1 25.82 27.81 36.15 21.3 2.7 24.8 25.8 27.79 36.13 m 3 /ha/season 7556 7136 8563 9175 9881 12845 7579 7158 859 924 9912 12885 Water requirements for onion: Table (11) and Figure (5) illustrates the water requirements for onion as compared to the climatic potential in Marondera region, Zimbabwe; they also indicate water requirements during the growth cycle of onion from March to October under many irrigation systems. The analysis shows that in this region, the total seasonal quantities of water ranged between 8876 and 15977 m3/he/season. The daily needs range from 23.32 to 93.97 m 3 /hectare/day. The lowest values are obtained in May, but the highest values are in July for many irrigation systems. The values are ranged in order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 1 to 2 days during the growth season. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). Table 11: Water requirements (m 3 /hectare/day) of onion grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface Mar 24.69 23.32 27.98 29.98 32.28 41.97 Apr 39.77 37.56 45.8 48.3 52.1 67.61 May 52.52 49.6 59.52 63.77 68.68 89.28 Jun 55.27 52.2 62.64 67.12 72.28 93.97 Jul 5.77 47.95 57.54 61.65 66.4 86.32 Aug 46.53 43.94 52.73 56.5 6.85 79.1 Sep 4.7 38.44 46.13 49.43 53.23 69.2 Oct 25.91 24.47 29.36 31.46 33.88 44.4 m 3 /ha/season 9398 8876 1651 11412 1229 15977 21

Seasonal irrigation water requirements (m3/he/season)) 18 16 14 12 1 8 6 4 2 Sub-surface Siphon Surface Onion Cabbages Tomatoes Spinach Covo Chinese Vegetables Cabbage Fig. 5: Water requirements (m3/hectar/season) of crops grown in Marondera region, Zimbabwe. Water requirements of cabbages: Table (12) and Figure (5) show the water requirements of cabbages grown in Marondera region, Zimbabwe. The water requirements vary from May to October under many irrigation systems. The total seasonal quantities of water ranged between 6328 to 1139 m 3 /he/season. The daily needs ranged from 14.88 to 113.71 m 3 /hectare/day. The lowest values are obtained in May, while the highest values obtained in July for many irrigation systems. The values ranged in of order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 6 to 16 days during the growth season. Similar results were obtained by Robina et al. (27), Abdel-Rahman et al. (28)a,b and Abdel-Rahman et al. (21). Table 12: Water requirements (m3/hectare/day) of cabbages grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface May 15.76 14.88 17.86 19.13 2.6 26.78 Jun 37.1 34.96 41.95 44.94 48.4 62.92 Jul 45.7 43.16 51.79 55.49 59.76 77.68 Aug 66.88 63.17 75.8 81.22 87.47 113.71 Sep 5.88 48.5 57.66 61.78 66.54 86.5 Oct 25.91 24.47 29.36 31.46 33.88 44.4 (m 3 /ha/season 67 6328 7593 8136 8762 1139 Water requirements of tomatoes: Table (13) and Figure (5) present the water requirements for tomatoes in Marondera region, Zimbabwe, which vary from 19.22 and 82.62 m 3 /hectare/day, and the total seasonal quantities of water vary between 5728 and 1311 m 3 /he/season. The lowest values are in September, but the highest values are in November for many irrigation systems. The values are ranged in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 11 to 25 days during the growth season. Similar results were obtained by Gouyahali and El-Hassan (21); Some et al. (24) and Robina et al. (27). Table 13: Water requirements (m 3 /hectare/day) of tomatoes grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface Nov. 48.6 45.9 55.8 59.1 63.55 82.62 Dec 48.23 45.55 54.67 58.57 63.8 82 Jan 33.26 31.41 37.69 4.39 43.49 56.54 Feb 22.47 21.22 25.46 27.28 29.38 38.2 Sep 2.35 19.22 23.7 24.71 26.62 34.6 Oct 48.57 45.88 55.5 58.98 63.52 82.58 (m 3 /he/season 665 5728 6874 7365 7931 1311 22

Water requirements of spinach : Table (14) and Figure (5) present the water requirements for spinach in Marondera region, Zimbabwe, the water requirements for spinach, range from 16.48 to 1.97 m 3 /hectare/day, and the total seasonal quantities of water vary between 562 and 184 m 3 /he/season. The lowest values are obtained in August, but the highest values obtained in November for many irrigation systems. The values are ranked in the order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 5 to 12 days during the growth season. Similar results were reported by Robina et al. (27), Abdel-Rahman et al. (28)a,b and Abdel-Rahman et al. (21). Table 14: Water requirements (m 3 /hectare/day) of spinach grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface Nov. 59.4 56.1 67.32 72.12 77.67 1.97 Dec 33.55 31.69 38.3 4.74 43.88 57.4 Jan 24.94 23.56 28.27 3.29 32.62 42.41 Aug 17.45 16.48 19.77 21.19 22.82 29.66 Sep 33.92 32.4 38.44 41.19 44.36 57.67 Oct 48.57 45.88 55.5 58.98 63.52 82.58 m 3 /he/ season 5931 562 6722 723 7757 184 Water requirements of covo : Table (15) and Figure (5) present the water requirements for covo grown in Marondera region, Zimbabwe, which range from 16.98 and 1.97 m 3 /hectare/day. The total seasonal quantities of water vary between 531 and 9558 m 3 /he/season. Table 15: Water requirements (m 3 /hectare/day) of covo grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface Nov. 59.4 56.1 67.32 72.12 77.67 1.97 Dec 33.55 31.69 38.3 4.74 43.88 57.4 Jan 24.94 23.56 28.27 3.29 32.62 42.41 Feb 17.98 16.98 2.37 21.83 23.51 3.56 Sep 2.35 19.22 23.7 24.71 26.62 34.6 Oct 48.57 45.88 55.5 58.98 63.52 82.58 m 3 /he/season 5622 531 6372 6827 7352 9558 Water requirements of Chinese cabbage: Table (16) and Figure (6) present the water requirements for Chinese cabbage in Marondera region, Zimbabwe, range from 18.35 to 77.74 m 3 /hectare/day. The total seasonal quantities of water vary between 4586 to 8254 m 3 /he/season. The lowest values are obtained in October, which the highest values obtained in January for many irrigation systems. The values are ranged in order: sub-surface < drip < sprinkler < gated < siphon < surface irrigation systems. Irrigation intervals ranged from 1 to 18 days during the growth season. Similar results were reported by Robina et al. (27), Abdel-Rahman et al. (28) a,b and Abdel-Rahman et al. (21). Table 16: Water requirements (m 3 /hectare/day) of Chinese cabbage grown in Marondera region, Zimbabwe. Sub-surface Siphon Surface Nov. 27 25.5 3.6 32.78 35.31 45.9 Dec 31.46 29.71 35.65 38.2 41.14 53.48 Jan 45.73 43.19 51.83 55.53 59.8 77.74 Feb 35.95 33.95 4.74 43.65 47.1 61.12 Mar 24.69 23.32 27.98 29.98 32.28 41.97 Oct 19.43 18.35 22.2 23.59 25.41 33.3 m 3 /ha/season) 4855 4586 553 5896 6349 8254 Irrigation requirements: Irrigation requirements are equal to water requirements, but irrigation requirements are the actual and practical irrigation needs after subtracting the effective rainfall (that is, the amount of rainwater actually used by crops) during all growth stages of crops. Irrigation requirements: Irrigation requirements in and (Fig., 7) are the equal water requirements, but irrigation requirements are the actual irrigation needs after subtracting the effective rainfall (that is, the amount of rainwater actually used by crops) during all growth stages of crops. 23

16 Sub-surface Siphon Surface 14 12 1 (m3/hectar/season) 8 6 4 2 Onion Cabbages Tomatoes Spinarch Covo Chinese Cabbage Vegetables Fig. 6: Irrigation requirements (m 3 /hectar/season) of crops grown in Marondera region, Zimbabwe. 14 Sub-surface Siphon Surface 12 1 (m3/hectar/season) 8 6 4 2 Wheat Barley Maize Potatoes Sugar Beet Cowpea Soyabeans Sunflower Crops Fig. 7: Irrigation requirements (m3/hectar/season) of crops grown in and region, Zimbabwe. 24

Irrigation scheduling: Data in table (17) and Fig. (8) show that the irrigation intervals (days) of crops grown in and regions ranged from 1 to 21 for wheat, 1 to 21 for barley, 11 to 13 for maize, 5 to 12 for potatoes, 1 to 25 for sugar beet, 1 to 23 for cowpea, 1 to 25 for soybean and 1 to 24 days for sunflower during the growth seasons. Comparison between water requirements and irrigation requirements: An examination of the two figures shows that the effective rainfall attributed the water requirements during the entire growth cycle of tomatoes, spinach, covo and Chinese cabbage. This means that the water requirements for these crops are somewhat met by rainwater during October to April, and that irrigation is unnecessary in some months. Similar results were obtained by Robina et al. (27), Abdel-Rahman et al. (28)a,b and Abdel-Rahman et al. (21). Table 17: Irrigation water intervals (days) for studied crops under different irrigation systems in and regions, Zimbabwe. Wheat Barley Maize Potatoes Sugar Beet Cowpea Soybeans Sunflower D H D H D H D H D H D H D H D H Nov. 11 11 7 11 1 12 11 14 Dec 13 13 12 2 12 15 12 15 Jan 14 17 11 14 Feb 19 19 16 17 11 14 1 12 Mar 13 13 13 13 15 18 1 13 Apr 1 1 1 1 2 25 11 14 May 17 18 17 18 17 18 23 24 25 24 3 Jun 12 12 12 12 25 26 Jul 1 1 1 1 Aug 21 21 21 21 8 13 Sep 5 8 Oct 13 13 5 7 3 Nov. Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct 25 2 15 Days 1 5 Wheat Barley Maize Potatoes Sugar Beet Cowpea Soyabeans Sunflower Crops Fig. 8: Irrigation intervals (days) of crops grown under some irrigation systems in and region, Zimbabwe. 25

Sub-surface Siphon Surface m3/hectar/season 18 16 14 12 1 8 6 4 2 Water requirements Irrigation requirements Water requirements Irrigation requirements Water requirements Irrigation requirements Water requirements Irrigation requirements Water requirements Irrigation requirements Water requirements Irrigation requirements Onion Cabbages Tomatoes Spinach Covo Chinese Cabbage Fig. 9: Water requirements and Irrigation requirements (m3/hectar/season) of crops grown in Marondera region, Zimbabwe. Irrigation scheduling: Data in table (18) and Fig. (1) show that the irrigation intervals (days) of crops in Marondera region ranged from 1 to 2 for onion, 6 to 16 for cabbages, 11 to 25 for tomatoes, 5 to 12 for spinach, 8 to 25 for covo and 1 to 18 days for Chinese cabbage during the growth seasons Similar trends were reported by Dastane (1978), Doorenbos and Pruitt (1984), Brouwer et al. (1989) and Allen, et al. (1998). Table 18: Irrigation water intervals (days) for studied crops under different irrigation systems in and regions, Zimbabwe. Onion Onion Cabbages Tomatoes Spanich Covo Chinese cabbage Nov. 11 5 8 13 Dec 12 9 14 14 Jan 17 12 18 1 Feb 25 25 13 Mar 15 18 Apr 1 May 11 15 Jun 13 11 Jul 16 9 Aug 17 6 1 Sep 2 8 16 7 13 Oct 12 16 11 6 8 14 26

3 Nov. Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct 25 2 Days 15 1 5 Onion Cabbages Tomatoes Spinach Covo Chinese Cabbage Crops Fig. 1: Irrigation intervals (days) of crops grown under some irrigation systems in Marondera region, Zimbabwe. Conclusions and Recommendations: From previous results, we can conclude that the effective rainfall contributions in the water requirements during the entire growth cycle of tomatoes, spinach, covo and Chinese cabbage. This means that the water requirements for these crops are somewhat met by rainwater during October to April, and that irrigation is unnecessary in some months. The effective rainfall attributed the water requirements during the entire growth cycle of tomatoes, spinach, covo and Chinese cabbage. This means that the water requirements for these crops are some met by rainwater during October to April, and that irrigation is unnecessary in some months. The irrigation intervals (days) of crops in the studied regions ranged from1 to 21 for wheat, 1 to 21 for barley, 11 to 13 for maize, 7 to 2 for potatoes, 1 to 26 for sugar beet, 1 to 24 for cowpea, 12 to 31 for soybean and 12 to 3 days for sunflower during,1 to 2 for onion, 6 to 16 for cabbages, 11 to 25 for tomatoes, 5 to 12 for spinach, 8 to 25 for covo and 1 to 18 days for Chinese cabbage during the growth seasons. The trend shows that irrigation requirements for maize in this region are met particularly by the amount of rainwater which is available from January March to crops. Rainy season tendency continues from October until March. Irrigation needs to grow until the end of the growth cycle, as shown by the curve. Table shows that the rainfall exceeds superior the water requirements during the entire growth cycle of maize from January to March. This means that the water requirements for maize are fully met by rainwater during this period, and that irrigation is unnecessary. The lowest values obtained in December, but the highest values obtained in November for many irrigation systems. Irrigation intervals ranged from 15 to 18 days during the growth season. Similar results were obtained From previous results, we conclude that the effective rainfall contributions in the water requirements during the entire growth cycle of tomatoes, spinach, covo and Chinese cabbage. This means that the water requirements for these crops are some met by rainwater during October to April, and that irrigation is unnecessary in some months. 1- Using Sub-surface, drip, sprinkler, gated and siphon irrigation systems can respectively save up to 44%, 41%, 33%, 28% and 23% of water as compared to surface irrigation system. 2- Further studied along these lines, determine the decreasing value in irrigation requirements that give an acceptable decreasing in yield for different crops. References Abdel-Rahman, G., S.H. Seidhom and Some, Leopold. 21. Soil and water relationships of some crops in Sahel-Dori, Burkina Faso. American-Eurasian J. Agric. & Environ. Sci., 7(3): 289-297. Abdel-Rahman, G., S.H. Seidhom, A.M. Talaat and Some, Leopold, 28a. Water requirements of some crops in Bobo-Dioulasso, Western region of Burkina Faso. J. Applied Sci. Res., 4(12): 1658-66. 27

Abdel-Rahman, G., S.H. Seidhom, A.M. Talaat and Seidhome, Leopold, 28b. Soil water balance of some crops in Bobo-Dioulasso, Western region of Burkina Faso. J. Applied Sci. Res., 4(12): 1667-77. Allen, R.G., L.S. Pereira, D. Raes and M. Smith, 1998. Crop evapotranspiration. Guidelines for computing crop water requirements. Irrig. & Drain. Paper, No. 56, FAO, Rome, Italy. Ayers, R.S. and D.W. Westcot, 1976. Water quality for agriculture. Irrig. & Drain. Paper No. 29, FAO, Rome, Italy. Brouwer C., K. Prins and M. Heibloem, 1989. Irrigation Water Management: Irrigation Scheduling, Training manual No. 4, FAO, Rome, Italy. Dastane, N.G., 1978) Effective rainfall in irrigated agriculture. FAO Irrigation and Drainage Paper, FAO 25, Rome, Italy. Doorenbos, J. and W.O. Pruitt, 1984. Crop water requirements. Irrig. & Drain. Paper No. 24, FAO, Rome, Italy. Gouyahali Son, and B. El-Hassan, 21. Problems of crop establishment in West Burkina Faso. I World Congress on Conservation Agriculture, Madrid, 1-5 October. Jensen, M.E., R.D. Burman and R.G. Allen, 199. Evapotranspiration and irrigation water requirements. ASCE, American Society of Civil Engineers. 7, New York, NY. Rhoades, J.D., 1984a. Reusing saline drainage waters for irrigation: A strategy to reduce salt loading of rivers. In: Salinity in Watercourses and Reservoirs, R.H. French (ed). Proc. 1983 Internat. Symp. on State-ofthe-Art Control of Salinity, 13 15 July 1983, Salt Lake City, Utah. Ann Arbor Science, pp: 455 464. Robina, W., M. Florent and M. Giovanni, 27. Actual Crop Water Use in Project Countries. A Synthesis at the Regional Level. The World Bank Development Research Group. Sustainable Rural and Urban Development Team, Policy Research Working, 4288. Smith, M., 1992. CROPWAT. A computer program for irrigation planning and management. Irrig. & Drain. Paper, No. 46, FAO, Rome, Italy. Some, L., Y. Dembele, M. Ouedraogo, M. Some, K. Bernadette, L. Faustin and Sh. Sangare, 24. Crops and soil water balance study with the CROPWAT model in Bobo-Dioulasso, BURKINA FASO. Institut De L environnement Et De Recherches Agricoles (INERA). 28