THE MUPFURE CATCHMENT

Table of contents:

THE MUPFURE CATCHMENT ...... 1

1 DESCRIPTION OF THE STUDY CATCHMENT...... 1

2 GEOLOGY AND RELIEF ...... 3

3 SOILS ...... 5

4 TEMPERATURES...... 6

5 RAINFALL ...... 7

6 REFERENCE POTENTIAL EVAPORATION ...... 9

7 LAND COVER ...... 9

8 LAND CLASSES ...... 10

9 CROPPING PRACTICES...... 11

10 RUNOFF...... 12

11 WATER CONSUMPTION...... 13

12 WATER RIGHTS...... 14

13 REFERENCES ...... 15

1 Description of the Study Catchment

The Mupfure River stretches for about 224 kilometres from 31o 15¢E, 18o 22¢S at its source up to 29o 25¢ E, 17o30¢S at the confluence with Sanyati River (Fig1). The catchment area covers 11 866 square kilometres. The source of Mupfure River is located along the central watershed of in the Chiota Communal Lands. The Department of Water Development has divided Zimbabwe into six hydrological zones, A to F, and the Mupfure River falls within Hydrological Zone C which comprises areas drained by the Sanyati and Manyame Rivers, and ultimately draining into the Zambezi River. The Mupfure catchment has been sub-divided into 4 hydrological sub-zones which are CUF1, CUF2, CUF3 and CUF4 (Fig 2).

Sub-zone CUF4 is found on the upper part of the catchment, and the major rivers occurring in this part are Muda, Mtsike, Nyachidzi, Marirangwe, and Nyonda Rivers. Sub-zone CUF3 stretches from downstream of Beatrice to the Mupfure Seruwe confluence. The major rivers occurring in this region are Doronanga, Nyundo, Nyakondowe, Nyangweni, and Chirundazi Rivers. The Lower Mupfure Catchment area is drained by the Washanje, Susuji, Chakari, and Nyabongwe Rivers.

Figure 1: The Mupfure Catchment

26 28 30 32 - 1 6

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26 28 30 32

a b e m w ha o i h h Kanzam#ba B.C C C ma ite Ch Angwa South #Obva Chitom borwizi

Mupfure WaMsha#nzjezuru Zim# bari Sachuru nje # sha Wa Zumbara B.C Chirau M#urindagomo St Rupperts Mission Ma gondi # Marevanani Zvimba Masiyarwa ri # # enji Zo wa Ch #Madzorera C he N gu Musengezi Musengezi y tu a 6 # b o Umfuli Marshall Hartley n Museng ezi g w B S i # e h ri Dombwe Chakari u r # # u Makwiro e s w Hartley h g R n u a u r S r n Large Scale Comm ercia l Fa rm s e i g u ru r u w a # e M Gadzema # Marirangwe Dalny Mine o # # e b C Selwous ru im Chib#ero h upfure h e a M e S C w k g a e # n r Chegutu k i S a i

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e # Reynold a Mupfure Centres n Ringa SSCFA i Communal Area Safari Area LSCFA Recreational Park

Figure 2: The Mupfure Hydrological Sub-zones

120000 160000 200000 240000 280000 320000

8080000 8080000

e a ow b h am C ih Ch a N em hit C

W E

M CUF1 u p hanje fu e Was r anj S e sh Wa je an ash W 8040000 8040000

N y Musengezi S usengezi a M h b o u

r n g u w s h B e u ir r i

u Biri R u n S g Sh e e u u CUF2 w r r u uw u e r e sh S ur o u b zi C m e d h i y i upfure h i h a M c w k C a a a y r y e N i S N w h g i 8000000 8000000 u n z a r r d u i i e h s r ik c ts h CUF3 a u u a r M y M u N C h hivake i C r u N n y D d u o a nd r z o a i n 'a CUF4 idi n hib g C a Mup N fure

y

a

n I n g y M w o n e d a n o v

i u

r

a

7960000 7960000

50 0 50 100 Kilometers

120000 160000 200000 240000 280000 320000

2 Geology and Relief

There are two major relief regions within the Mupfure Catchment which are the highveld and the middleveld (Fig 3). The highveld which consists of land with altitude from 1 200 metres to 1 560 metres above sea level and occurs mostly in the mid to upper parts of the catchment. The middleveld has altitude ranging from 900 to 1 100 metres and this occurs mostly on the lower part of the catchment.

The middleveld stretches from Chegutu to the confluence of Mupfure and Sanyati river ranging in height from 900 metres to about 1 100 metres above sea level. The mid and upper Mupfure catchment are characterised by slopes which range from 0° to 2° with the exception of river banks especially along the Mupfure River. The average slope values along the Mupfure River are in the range of 2.5° to 3.2°. The maximum slopes along the river are 3.4°. Thus more than 90% of the mid and upper Mupfure catchment is characterised by slopes less than 2°. This covers the following areas: Chiota, Beatrice, Mhondoro, Chegutu, Musengezi, and up to Chegutu.

The Selous and the Makwiro area the slopes range from 3° to a maximum of 10°. This is in areas mainly along the Great Dyke. South of Selous the slopes are moderately steep with the steepness gradually decreasing from 9° to 3°. In the Lower Mupfure Catchment area there are steep slopes ranging from 9° to over 15°. The Susuji River which drains part of the Magodi Communal Lands on the right bank of the Mupfure River is characterised by rugged terrain. The average slopes along this river are around 19’’ degrees. One of the prominent relief features of this area is the Cheka- Wakasunga-Bete Ridge, which has a NNE-SSW alignment. Slopes along this ridge range from 9° to 30°. Moderately steep slopes of around 9° occur along river valleys such as those of Nyundo and Nyangweni Rivers. The upper catchment and parts of the mid catchment have numerous dambos occurring within them. These are seasonally waterlogged bottomlands. Dambos in the commercial farms are found in nearly their natural state with limited degradation. This is because the farms have been subjected to limited and controlled grazing pressure, have little or no cultivation and there are numerous dams that help maintain the water table. On the other hand, in communal areas dambos have been subjected to heavy pressure from humans and livestock, have been overgrazed, cropped and trampled. As such most of the dambos are degraded and eroded. Dambos as such are more common around areas such as Mahusekwa and Mudzimurema centres in the upper catchment and around Kutama and in Zvimba Communal Lands in the lower catchment and are characterised by cultivation (vegetable gardens) and livestock grazing in these communal areas.

Figure 3 Relief of the Mupfure Catchment

N Legend 775 - 805 1168 - 1198 805 - 836 1198 - 1229 836 - 866 1229 - 1259 866 - 896 1259 - 1289 896 - 926 1289 - 1319 926 - 956 1319 - 1350 956 - 987 1350 - 1380 987 - 1017 1380 - 1410 1017 - 1047 1410 - 1440 1047 - 1077 1440 - 1470 1077 - 1108 1470 - 1501 1108 - 1138 1501 - 1531 1138 - 1168 1531 - 1561 (altitude above sea level in metres)

M iddl eveld

Highveld

40 0 40 Kilometers

The major geological formations found in the Mupfure Catchment include the Greenstone Belt, granitoids, Great Dyke rocks, the Lomagundi and the Piriwiri Group of rocks (Fig 4). The Greenstone Belt (early precambrian) comprises metasediments, metavolcanics, and ultramafic lavas that cover about 38% of the catchment. These occur around Beatrice and in the south-western part of the catchment around Chegutu, Golden Valley, and Chakari (Fig 4). The granitoid group of rocks include granites and gneisses of various ages, and these cover about 39% of the catchment. They occur mostly in Chiota, Mhondoro, Selous, Musengezi and Zvimba Communal Lands. One of the prominent geological features of this catchment is the Great Dyke which is a secondary tectonic feature that runs north-south across the catchment. This dyke is rich in minerals such as chromite, platinum, nickel, asbestos, and magnesite. The Lomagundi and the Piriwiri groups of rocks (mid precambrian) consist of dolomites and phyllites which occur mostly in the north-western part.

Figure 4: Geology of the Mupfure Catchment

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000 8 0 0 0 8 0 0 0 0 8 0 0 0 8

Mupfure Geology 8

0 Bulawayan and Shamvan group 0 0 6 0 0

0 Bulawayan group 0 6 0 0 0

8 Deweras group Dolerite Felsites and porphr 8

0 Granite 0 0 4 0 0

0 Great Dyke 0 4 0 0 Kalahari aeolian sands 0 8 Karroo basalt Karroo sandstone 8

0 Lomagundi group 0 0 2 0 Piriwiri group 0 0 0 2 0 0 0 8 8 0 0 0 0 0 0 0 0 0 0 0 0 8 N 7 0 9 0 8 0 0 0 0 8 0 9 0 7 7 0 9 0 6 0 0 0 0 6 0 9 0 7 40 0 40 80 Kilometers

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000

3 Soils

The Mupfure Catchment is composed mainly of the following soil groups: the fersiallitic, vertisol, lithosol, paraferrrallitic, othoferrallitic, and the lithosol groups. According to Thompson (1965) in Nyamapfene (1991) the soil classification system used in Zimbabwe as developed by Thompson (1965) is composed of four taxonomic levels namely the order, the group, the family, and the series. The lithosol group as found in the Mupfure Catchment belongs to the amorphic order which is reserved for those soils in which a low degree of profile development is a characteristic. The vertisol group belongs to the calcimorphic order, which is characterised by soils that are ralatively unleached and generally have large reserves of weatherable minerals with high base saturation and clay fractions predominantly active. This results in cohesive soils because of the clay content of the soils. The fersiallitic, orthoferralliti, and the paraferrallitic groups belong to the kaolinitic order, which is characterised by moderately to strongly leached soils.

The lithosol group of soils includes all soils with a depth less than or equal to 25 centimetres. They occur generally extensively on flat areas in low rainfall areas, particularly those areas underlain by rock which is relatively resistant to weathering. In the Mupfure Catchment these occur in the lower catchment area (Fig 5). On the other hand, most of the vertisols are moderately deep, generally ranging in depth from about 80 centimetres to a metre or just slightly more than a metre. These are found in a small portion in the upper catchment area south of the Mupfure River. The clay content in all Zimbabwean vertisols is high (well over 60%), and as such are often subject to hydromophy.

The fersiallitic group of soils all tend to be acidic with those derived from siliceous parent materials being more acidic than those from mafic materials. The main soil forming processes have been the accumulation of clay and to a significant extent, the accumulation of sesquioxides and leaching of bases. In the catchment area the fersiallitic group of soils are mainly confined in the mid catchment area. The paraferrallitic soils of Zimbabwe are almost exclusively derived in situ from granite parent rock and are predominantly sandy hence relatively highly leached in high rainfall areas (mean annual precipitation greater than 800 millimetres). These are predominant in the upper catchment are and they have at least 5 % weatherable minerals present in the system. The orthoferrallitic group of soils occur in the upper catchment have profiles which are normally very deep being not less than two metres in depth and exhibit a very fine crumb structure which is weakly developed. The soils are largely the result of deep weathering of the underlying rock followed by intense leaching of bases in high rainfall areas. Porosity is very high and the soils have relatively high clay content. Most of the soils are highly coloured due to the high oxide content and their extremely good internal drainage. Figure 5 shows the distribution of soil types in the Mupfure Catchment:

Figure 5 Soils of the Mupfure Catchment

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000 8 0 0

0 N 8 0 0 0 0 8 0 0 0 8 Mupfure Soils 2 - Lithosol Group 5M - fersiallitic Gr 8 0 0

0 5M - fersiallitic gr 6

0 2 - lithosol group 0 0 0

6 5S - fersiallitic gr 0

0 3B - vertisol group 0 8 4E - siallitic group 5S/2 - Fersiallitic 5E - Fersiallitic gr 5S/5A - fersiallitic 8 0 0

0 5E - fersiallitic gr 5X - fersiallitic gr 4 0 0 0 0

4 5E/3E - fersiallitc 5X/3X - fersiallitic 0 0 0 8 5G - fersiallitc gro 6G - paraferrallitic 5G - fersiallitic gr 7G - orthoferralliti 8 0 0 0 2 0 0 0 0 2 0 0 0 8 8 0 0 0 0 0 0 0 0 0 0 0 0 8 7 0 9 0 8 0 0 0 0 8 0 9 0 7 7 0 9 0 6 0 0 0 0 6 0

9 40 0 40 Kilometers 0 7 7 0 9 0 4 0 0 0 0 4 0 9 0

7 120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000

4 Temperatures

Fig 6 shows the variation in maximum and minimum temperatures throughout the year. The highest temperatures are experienced during the September to November period. The May to early August period is considered to be the cool season during which relatively low temperatures occur. Frost does occasionally occur in some parts of the catchment.

Figure 6: Monthly Temperature Variations

Average Monthly Temperatures (Mhondoro)

35 30 25 20 Max 15 Min 10 5 0 JUL AUG SEP OCT NOV DEC JAN FEB MAR APR MAY JUN

5 Rainfall

There are 14 rainfall stations within the Mupfure Catchment (Fig 7). The density of these stations varies from 1 rain gauge per 266 sq km in the lower part of the catchment to 1 gauge per 46 sq. km in the upper catchment (Table 1)

Table 1: Density of Rain gauges in the Mupfure Catchment

Number of Rain gauge Rainfall Density (gauges Zone Area (km2) Stations per km2) CUF1 403.53 3 135 CUF2 265.81 1 266 CUF3 251.65 5 50 CUF4 276.50 6 46

Figure 7 The location of rainfall stations in the Mupfure Catchment

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000

8080000 8080000 N

W E

S 8060000 8060000

Zimbari #

8040000 St Ruppets 8040000 #

8020000 8020000

Dalny Mine Selous Carnock# # # Chibero # Dunolly 8000000 Chegutu # 8000000 #

Burnbank # Beatrice # Mubayira Mahusekwa 7980000 # # 7980000 # Ensidale Poltimore #

Matana School 7960000 # 7960000

7940000 7940000

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000

Rainfall increases in general from the west to the east with increase in altitude. Parts of the lower catchment receive about 670 mm of rainfall per year (Table 2). This increases to about 700 mm in the middle part of the catchment. The highest rainfall occurs in north-eastern parts which get about 800 mm per year.

Table 2 Rainfall stations in the Mupfure Catchment

Station Period Mean Annual Rainfall

(mm) Beatrice 1949/50-93/94 709 Burnbank 1949/50-93/94 687 Chegutu 1909/10-95/96 748 Chibero 1959/60-94/95 717 Dalny Mine 1949/50-94/95 727 Dunolly 1933/34-86/87 751 Mahusekwa 1949/50-86/87 736 Matana School 1954/55-86/87 724 Mubayira 1962/63-94/95 731 Selous 1971/72-95/96 747 St Ruppets 1971/72-94/95 746 Zimbari 1964/65-94/95 670 Ensidale 1970/71-96/97 615 Carnock 1970/71-96/97 784 Poltimore 1979/80-95/96 718

Rainfall varies greatly from one year to another, and the coefficient of variation of annual rainfall is as high as 30%. Fig 8 shows the considerable variability in the annual rainfall at Beatrice. During the rainy season which stretches from mid-November to March, rainfall often occurs in the form of 10 to 15 day wet spells that are followed by dry spells of similar duration. The rain comes mostly in the form of convective thunderstorms. The rest of the year from May to early November is dry (Fig 8).

Figure 8 Annual Rainfall Variability.

Annual Rainfall Variability (daily values)

60

50

40

30

20

Rainfall (mm) 10

0 7/1/70 1/1/71 7/1/71 1/1/72 7/1/72 1/1/73 7/1/73 1/1/74 7/1/74 1/1/75 7/1/75 1/1/76 7/1/76 1/1/77 7/1/77 1/1/78 7/1/78 1/1/79 7/1/79 1/1/80 7/1/80

6 Reference Potential Evaporation

There is only one station at which evaporation is measured within the Mupfure catchment. This is at Chibero. The other station close to the study area is Kutsaga Tobacco Research Station just outside Harare. Fig 9 shows the mean monthly evaporation rates measured using an A-pan. This shows that evaporation rates are considerably high ranging from 150 to 250 mm per month. The average annual evaporation rates vary from about 1900 mm in the lower parts of the catchment to 1800 mm in the upper part of the catchment.

Figure 9 Monthly Pan Evaporation

Potential Evaporation

300

250 200

150

100

50

0 Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep

7 Land cover Kutsaga Chibero Average

The various types of land cover occurring within the Mupfure Catchment were determined from a classification of a Landsat TM image of April 1998. The dominant land cover are woodlands that occupy 53% of the catchment. This is followed by cultivated lands that cover 27% of the area. Areas under bush cover 13% (Fig 10 and Table 3)

Table 3 Land cover types in the Mupfure Catchment area.

Landuse Types % Of Area Covered Woodland 53.20 Cultivation 27.47 Bushland 12.72 Grassland 1.76 Water bodies 1.77 Plantations 0.40 Settlements 0.36 Rock outcrops and Mine dumps 0.20 Natural Moist Forest 0.03

Most of the woodlands occur in areas under large and small scale commercial farming such as the Selous, Gadzema and Msengezi in the mid catchment, and Angwa South and Chitomborwizi in the lower catchment area. Cultivated areas commonly occur in communal areas.

Figure 10 Types of Land Cover Occurring within the Mupfure Catchment

30 31

N Mu_woody_dd Natural Moist Forest (0.03%) Plantation (0.40%) Woodland (53.20%) Bushland (12.72%) Wooded Grassland (3.08%) Grassland (1.76%) Cultivation (27.47%) Rock Outcrop & Mine Dump (0.20%) Waterbody (0.77%) Settlement (0.36%)

-18 -18

30 31

8 Land Classes

There are three major land classes occurring within the study area, and these are communal areas, small scale commercial farming areas, and large scale commercial farming areas. Table 4shows the area covered by the various land classes.

Table 4 Major Land Uses in the Mupfure Catchment

Land Tenure Name 8.1.1.1.1.1.1 A r e a in k m 2

Communal Area Chihota 430 Communal Area Chirau 328 Communal Area Magondi 514 Communal Area Mhondoro 1115 Communal Area Mupfure 619 Communal Area Zvimba 149 LSCFA Angwa South 759 LSCFA Large Scale Commercia l Farms 5195 Recreational Park Umfuli 143 Resettlement Area Acton 154 Resettlement Area Chegutu 6 125 Resettlement Area Musengezi 163 Resettlement Area Reynold 144 Resettlement Area Ringa 38 Resettlement Area Rutara Hills 17 Resettlement Area Sachuru 253 Safari Area Hartley 301 SSCFA Chenjiri 133 SSCFA Chimbwanda 54 SSCFA Chitomborwizi 250 SSCFA Marirangwe 90 SSCFA Muda 49 SSCFA Musengezi 321 SSCFA Zowa 212

9 Cropping Practices

The major crops cultivated in communal areas are maize, groundnuts, sunflowers, cotton and sorghum. Within communal lands cultivated lands are tilled using mostly ox drawn ploughs which loosen the soil to a depth of about 15 to 20 cm. On the other hand, in the commercial farming areas tractors are used in the ploughing or disking of the land. These loosen the soil to a maximum depth of around 30 to 45 cm. The major crops grown in large scale commercial farming are tobacco (flue cured) and maize. Irrigation of tobacco is undertaken in order to supplement rainfall. Irrigation of winter wheat is also undertaken in large scale commercial farming areas. In the small-scale commercial farming areas there is a mixture of both tobacco (barley - air cured), cotton and maize farming. Most of the crops in these areas are dependent on the rainfall received during the rainy season.

Most of the maize is planted by the 15th of November but sometimes planting goes on up to the 25th of December in the communal areas. Harvesting of maize is usually done 5 to 6 months later depending on the crop variety. In the lower rainfall areas sorghum is usually planted with the first rains and it takes about 60 days to flower and is harvested 3 to 4 months later when it dries. Groundnuts are also planted with more or less the first rains and takes 110 to 150 days to mature, harvesting of which is done 4 to 5 months after planting. As for cotton, land has to be ready for planting by the middle of October since it has a long growing season of 180 to 280 days. Thinning has to be done before November and harvesting normally takes place for 12 to 16 weeks in March up to July or August.

It is estimated that 26 600 hectares of land is under irrigation in all the large scale commercial farming areas, while 113 hectares are under small holder irrigation schemes. The existing small holder irrigation schemes are Hamilton Mills, Johannadale, Madzongwe, Shamrock, and Mahusekwa. The estimated water usage for irrigation is 266000 ML for the large scale commercial farming area, and 1130 ML for small holder irrigation schemes. The total amount of water granted to water rights belonging to LSCFA is 223 856 ML. The proportion of irrigated land under different crops are shown in Table 5 below.

Table 5 Proportion (%) of Irrigated Land Under Different Crops.

Crop Beatrice Norton Gadzema Selous Suri Suri Mupfure North Maize 17 12 6 11 27 10 Wheat 1 0 0 20 11 0 Tobacco 21 21 31 26 2 53 Cotton 0 0 32 5 23 0 Soya bean 0 42 15 11 28 0 Others 60 25 16 27 9 37 Total 100 100 100 100 100 100

Tobacco occupies the greatest proportion of land under irrigation. However, irrigation of tobacco is mostly required during the establishment of tobacco seedlings in the early summer period.

10 Runoff

There are nine flow-measuring stations along the Mupfure River and these are equipped with automatic recorders (Fig 11). Table 6 below shows the stations and their catchment areas.

Table 6 River Flow Measuring Stations

Code Location Catchment Area Period of Record (sq km) C12 Twyford Weir 5180 1950/51-95/96 C65 Upper Seigneury U/S 4140 1964/65-95/96 C44 Lower Seigneury D/S ----- 1988/89-94/95 C67 Maynard Weir U/S 3650 1966/67-95/96 C70 Beatrice 1215 1969/70-95/96 C78 Johannadale 8240 1990/91-94/95 C107 Mahusekwa D/S 129 1989/90-95/96 C108 Mahusekwa D/S 122 1989/90-95/96 C84 Copper Queen 12100 1990/91-95/96

Runoff is highly seasonal as is characteristic of most rivers in Zimbabwe. Flows start to increase in late November. High flows are experienced during the December to February period. Afterwards flows decrease, and most rivers dry up during the July to November period (Fig 12). The duration of periods with zero flows varies from 70 to 155 days per year along the Mupfure River. Runoff is highly variable, and the coefficient of variation being 130% at Beatrice The mean annual runoff varies from 103 mm in the upper part to 50 mm in the lower part of the Mupfure Catchment.

Fig 11 The location of the flow measuring stations 120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000 8 0 0 0 8 0 0 0 0 8 0 0 0 8 N e w ba ho am C ih h 8 C W E 0 a 0 0 m 6 te 0 %% hi 0 0 C 0 6 0

0 S 0 8

M u p fu r je e han Washanje 8

0 s 0 Wa 0 4 0 0

0 e 0 nj 4 ha 0 0 as 0

8 W

% Mupfure Flow Gauges 8

0 N Muse Major Rivers 0 y ngezi 0 Musengezi 2 a

0 b 0

S

0 o 0 n h 2 g u 0

r 0 w % 0 u B

8 e s i h ri %

u

r u Biri R u e n S w S g h % u e 8 u u r r 0 e u 0 ru S w 0 % 0 % sh e

0 u 0 % r % o 0 % 0 u % b i e z 0 C m d 0 i y i 0 h % % h i h 0 a w 8 % C c k a a a y r y e i N N S w g h % i u n z a r d % r i u % i e s r h ik

h c s 7 a ut u a 0 9 M y M r %

0 u % 8 % N 0 0

0 hivake 0 C % C 8 h 0

9 i N 0 r u y D 7 un o n d r i d o a ibid a n Cih z 'a bid i n hi g %C a M%up N fure 7

y

a 0 I 9 n n 0 6 g y M

0 w o 0

0 n 0 a e d

n v 6 o 0 u i 9 0 r

a 7 30 0 30 60 Kilometers

120000 140000 160000 180000 200000 220000 240000 260000 280000 300000 320000

Fig 12 Mean Monthly Flows at C70

20 18 16 14 12 10 8 flows (mm) 6 4 2 0 OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP

11 Water Consumption

There are no records of the amount of water consumed for domestic purposes in communal areas. An estimate of this consumption can be made using the size of the population within the Mupfure Catchment. The 1992 Census found that there were about 350 000 people within this catchment. If it is assumed that the average water consumption is 25 litres per capita per day, then the amount of water used for domestic purposes is about 3 million cubic metres per year.

The amount of water consumed for urban, industrial, and mining (UIM) purposes can be estimated form the records of the Department of Water Development. Table 7 below shows the amount of water consumed at various centres that are supplied with water by this department. Table 7 Water Consumption at Main Centres

Centre Water Source Total Water Consumption (ml/year) Beatrice Borehole + River 148 Chakari Borehole 38 Changafuma Chegutu Town 35 Chibero College Borehole + Dam 136 Chegutu Dams 600 Ensidale Borehole 28 Gadzema Borehole 14 Kamhonda Clinic Borehole 6 Kinzamba Borehole 2 Mahusekwa Dam 54 Msengezi Secondary School Borehole 44 Msengezi Ressettlement Scheme Borehole 3 Mubayira Borehole 124 Selous Borehole 34 Ringa Borehole 16

12 Water Rights

According to the legislation in Zimbabwe, anybody who wishes to user water for non-domestic purposes has to be granted a water right or permit to do so. This requirement is also applicable to towns, mines, missions, and similar institutions that abstract and distribute water to residents for domestic purposes. The amount of water allocated to water right holders can be used as an indicator of the amount of water being used. This has its limitation in that water right holders do not always utilize their full allocations, and some may illegally exceed these allocations. Table 8 shows the number of water rights and volumes of water that have been allocated to various types of water users within the Mupfure Catchment.

Table 8 Amount of water allocated to various Sectors

CUF1 Number of Water Rights Amount of Water Total Commitment Commitment (ML) (ML) Storage Abstraction Storage Abstraction LSCFA 12 11 9293 1360 10653 Communal Areas 0 5 0 220 220 Mines 1 0 1409 0 1409 Government 0 0 0 0 0 Roads 0 0 0 0 0 Total 13 16 10702 1580 12282 CUF2 LSCFA 150 82 77221 21791 99012 Communal Areas 0 0 0 0 0 Mines 0 2 0 68 68 Government 6 2 11840 11205 23045 Roads 0 2 0 0 0 Total 156 88 89061 33064 122125 CUF3 LSCFA 77 57 61371 8210 69581 Communal Areas 3 2 571 62 633 Mines 0 1 0 6 6 Government 5 0 12032 0 120032 Roads 0 6 0 6 6 Total 85 66 73979 8284 82263 CUF4 LSCFA 92 82 34641 9969 44610 Communal Areas 0 0 0 0 0 Mines 0 0 0 0 0 Government 0 0 0 0 0 Roads 0 14 0 0 14 Total 92 96 34641 9983 44624 Source: Mazvimavi (1998) The large scale commercial farming sector (LSCFA) have most of the water allocated to water right holders. Government also has substantial amounts of water allocated to it, which is used mostly for water supply to the town of Chegutu.

13 References

Bonifacio, R. and D.I.F. Grimes, (1998), Drought and flood warning in southern Africa. IDNDR Flagship Programme - Forecasts and Warnings, UK National Coordination Committeed for the IDNDR, Thomas Telford, London.

John C Rodda (1985) Facets of Hydrology John Wiley and Sons Ltd, London UK.

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