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Chapter 2
Zimbabwe's natural regions and farming systems


Natural regions

Zimbabwe is divided into five agro-ecological regions, known as natural regions (Figure 1), on the basis of the rainfall regime, soil quality (Figure 2) and vegetation among other factors. The quality of the land resource declines from Natural Region (NR) I through to NR V (Moyo, 2000; Vincent and Thomas, 1961). Table 1 describes these natural regions and their farming systems.

Figure 1
Natural regions of Zimbabwe


Figure 2 Dominant soil map of Zimbabwe

Original scale 1:5 million
Source: DSMW-FAO-Unesco

Natural Region I

This region lies in the east of the country. It is characterized by rainfall of more than 1 000 mm/year (most of which falls throughout the year), low temperatures, high altitude and steep slopes. The country's timber production is located in this region. The plantations are owned mainly by the State through the Forestry Commission and by multinationals. There are several small owner-operated plantations and sawmills. NR I is ideally suitable for intensive diversified agriculture and livestock production, mainly dairy farming. Common crops are tropical crops such as coffee and tea, deciduous fruits, such as bananas and apples, and horticultural crops, such as potatoes, peas and other vegetables. Flowers, such as proteas (Proteaceae spp.), are grown for export.

TABLE 1
Description of the Natural regions of Zimbabwe

Natural
Region

Area
(000 ha)

% of total land area
(%)

Annual rainfall

Farming Systems




(mm)


I

613

1.56

> 1 000. Rain in all months of the year, relatively low temperatures

Suitable for dairy farming forestry, tea, coffee, fruit, beef and maize production

II

7 343

18.68

700-1 050. Rainfall confined to summer

Suitable for intensive farming, based on maize, tobacco, cotton and livestock

III

6 855

17.43

500-800. Relatively high temperatures and infrequent, heavy falls of rain, and subject to seasonal droughts and severe mid-season dry spells

Semi-intensive farming region. Suitable for livestock production, together with production of fodder crops and cash crops under good farm management

IV

13 010 036

33.03

450-650. Rainfall subject to frequent seasonal droughts and severe dry spells during the rainy season

Semi-extensive region. Suitable for farm systems based on livestock and resistant fodder crops. Forestry, wildlife/tourism

V

10 288

26.2

< 450. Very erratic rainfall. Northern low veldt may have more rain but the topography and soils are poor

Extensive farming region. Suitable for extensive cattle ranching. Zambezi Valley is infested with tsetse fly. Forestry, wildlife/tourism

Source: Adapted from Moyo, 2000; Vincent and Thomas, 1961.

Natural Region II

This region is located in the middle of the north of the country. The rainfall ranges from 750 to 1 000 mm/year. It is fairly reliable, falling from November to March/April. Because of the reliable rainfall and generally good soils, NR II is suitable for intensive cropping and livestock production. It accounts for 75-80 percent of the area planted to crops in Zimbabwe. The cropping systems are based on flue-cured tobacco, maize, cotton, wheat, soybeans, sorghum, groundnuts, seed maize and burley tobacco grown under dryland production as well as with supplementary irrigation in the wet months. Irrigated crops include wheat and barley grown in the colder and drier months (May-September). NR II is suitable for intensive livestock production based on pastures and pen-fattening utilizing crop residues and grain. The main livestock production systems include beef, dairy, pig and poultry. Prior to 2000, the region was dominated by the large-scale farming subsector characterized by highly mechanized farms of 1 000-2 000 ha under freehold title and owner-operated. Following the agrarian and land reform programmes initiated in 1999/2000, a large proportion of the farms were subdivided into smaller units and allocated to new farmers under the A1 and A2 small-scale farming system.

Natural Region III

NR III is located mainly in the mid-altitude areas of the country. It is characterized by annual rainfall of 500-750 mm, mid-season dry spells and high temperatures. Production systems are based on drought-tolerant crops and semi-intensive livestock farming based on fodder crops. The predominant farming system is smallholder agriculture. Large-scale farming accounts for 15 percent of the arable land production, most of the land being used for extensive beef ranching (Roth, 1990). Smallholder agriculture in the communal farming areas is under relatively intensive cropping systems. The main crops are maize (the staple foodgrain) and cotton (a major cash crop). NR III is suitable for the production of groundnuts and sunflowers as cash crops.

Natural Region IV

NR IV is located in the low-lying areas in the north and south of the country. The characteristics of the region are: annual rainfall of 450-650 mm, severe dry spells during the rainy season, and frequent seasonal droughts. Although NR IV is considered unsuitable for dryland cropping, smallholder farmers grow drought-tolerant varieties of maize, sorghum, pearl millet (mhunga) and finger millet (rapoko). NR IV is ideally suitable for cattle production under extensive production systems and for wildlife production.

Natural Region V

NR V covers the lowland areas below 900 m above sea level in both the north and south of the country. The rainfall is less than 650 mm/year and highly erratic. Although NR V receives reasonable rainfall in the northern part of Zimbabwe along the Zambezi River, its uneven topography and poor soils make it unsuitable for crop production. Generally, NR V is suitable for extensive cattle production and game-ranching.

Although both NR IV and NR V are too dry for crop production, households on the communal lands in these regions grow grain crops (maize and millet) for their food security and some cash crops such as cotton. Crop yields are extremely low and the risk of crop failure is high in one out of three years (Rukuni and Eicher, 1994). Cattle and goat production are major sources of cash income.

Table 2 further subdivides the five NRs into 18 agro-ecological zones (AEZs) by including information on soils and on the probability of annual rainfall exceeding 500 mm.

Soil quality and fertility

Thompson and Purves (1978) give a comprehensive guide to the characteristics of factors determining the fertility of the soils of Zimbabwe. Generally, virgin soils in Zimbabwe are infertile and deficient in nitrogen (N), phosphorus (P) and sulphur (S). About 70 percent of Zimbabwe is covered with sandy soils, mostly derived from coarse granite. Sandy soils in the south are derived from gneiss. The northwest of the country has Triassic and Kalahari sands. Zimbabwe sandy soils are low in N, P, and S and in cation exchange capacity (CEC) owing to low clay and organic matter contents (Grant, 1967a, 1967b, 1970; Nyamapfene, 1981). In addition, the sandy soils are generally acidic. According to Grant (1970), many crops on granite sandy soils on the communal lands reveal multiple nutrient deficiencies of N, P and S as well as of magnesium (Mg) and potassium (K) and of micronutrients such as zinc (Zn).

S deficiency is endemic. Mg deficiency is more pronounced where the sandy soils are cropped using fertilizer NPK alone. Zn deficiency is encountered more in intensively cropped areas. The soils are inherently deficient in boron (B). Copper (Cu) deficiency occurs in irrigated lands. Generally, there is no iron (Fe) deficiency.

TABLE 2
Agro-ecological zones

NR

AEZ

Area

Probability rainfall > 500 mm Oct. to Apr.

Length of growing period

Physiographic region

Altitude

Erosion hazard

Dominant soils

pH topsoil

CEC

NPK

Available waterholding capacity



(million ha)

(%)

(days)


(m)





(me/ 100 g soil)



I

I

0.7

>90

170-200

Eastern Highlands

1 100-2 600

medium

red soil

Acrisols, Ferralsols

4.4-5.1

2.0-6.0

K var., N

high

II a

IIA

4.1

>90

140-170

Northern Highlands

1 100-1 800

variable

greyish brown sands and sandy loams derived from granitic rocks

Cambisols, Luvisols, Arenosols

4.0-4.3

1.5-5.0

K med., N

mod.-low

II b

IIB

1.8

80-90

120-150

Northern Highlands, NE & SE Middleveldt

1 100-1 600

variable

greyish brown sands and sandy loams derived from granitic rocks

Cambisols, Luvisols, Arenosols

4.0-5.0

1.0-3.0

K var., N

mod.-low

III

II(1)

0.7

70-90

100-130

Kalahari Sandveldt

1 100-1 200

medium

deep Kalahari sand

Arenosols

4.6-4.9

1.0-1.2

K med., N & P low

low


II(2)

1.4

70-80

110

Sanyati-Sengwa Basin SE Middleveldt

600-1 200

high

very shallow

Leptosols, Lixisols

4.5

3.0-4.0

K med.

low


IV(5)

7.6

40-65

100-135

NE

Middleveldt SE Middleveldt

600-1 200

variable

greyish brown sands and sandy loams derived from granitic rocks

Luvisols

4.4-4.8

2.0-5.0

K & P med.

low

V

V(2)

0.7

60

100-135

Zambezi Valley

600-900

high

very shallow

Leptosols




low


V(3)

0.5

30-40

70-100

SE Lowveldt

300-400

low

Vertisols

Vertisols

6.8

65-100


high


V(4)

1.5

40-60

100-130

Sanyati-Sengwa Basin

500-700

medium

brown loamy sands & loams

Luvisols, Solonetz




low-mod.


V(5)

3.9

40-60

70-100

SE Lowveldt

300-600

low-med.

Sands & sandy loams derived from granite & gneiss

Luvisols

6.0-7.0

20

K & P med.

low-mod.



3

<30

<70

SE Lowveldt

300-900

high

Variable

Leptosols, Luvisols

6.0-7.0

10-20


variable

Source: FAO & ACFD, 1999.

TABLE 3
Nitrogen percentage of different soil types

Texture

Total N (%)

Clays

0.10-0.15

Sands

0.02-0.05

Sandy clay loams

0.06-0.07

Sandy loams

0.04-0.07

TABLE 4
Fertilizer nutrient requirements of soils of different fertility status

Fertilizer nutrient

Nutrient status of the soil

Good

Medium

Poor

(kg/ha of fertilizer nutrient required)

N

up to 110

110-140

140-180

P

40-65

65-100

100-135

K

20-45

45-70

70-95

Source: AGRITEX, 1982.

As these soils are inherently of low fertility and subject to rapid depletion in fertility, regular applications of organic and inorganic fertilizers are necessary in order to obtain reasonable and sustainable yields. The soils need liming to correct soil acidity and then fertilizing to correct for low P and K levels.

The total N content of the soil varies greatly, being higher in higher rainfall areas than in lower rainfall areas, higher in wetland soils and heavy-textured soils than on sandy soils, higher in virgin soils than in cultivated soils, and lower in the subsoil than in the topsoil (Table 3).

Table 4 gives the nutrient requirements of soils of good, medium and low fertility status. Applications on a continuing basis are necessary for optimal economic production of most crops. However, for most of the farming households in the smallholder subsector, investment in soil fertility is low owing to financial constraints.

Characteristics and distribution of farming systems and farming units

Prior to 2000, there were four distinct farming systems or farming subsectors in Zimbabwe, determined by: agro-ecological factors, tenure systems, farm sizes, crop and livestock production systems, levels of technology use, management and income levels. The farming systems had also been determined by the political and historical development of the country during the 90 years of colonial and settler government. These systems were: communal lands, resettlement areas, small-scale commercial, and large-scale commercial (Table 5). The dominant subsectors, in terms of population size, area under production and agricultural output, were the large-scale commercial and the communal lands farming systems.

TABLE 5
Land tenure and characteristics of the farming systems

Farming system

Tenure and farming characteristics

Communal and resettlement

Communal land tenure, labour-intensive production system using ox-drawn implements, semi-commercialized

Large-scale commercial

Freehold title to land, highly mechanized, fully commercialized

Small-scale commercial

Leasehold title to land, labour-intensive production with little use of tractor-drawn implements, most production for the market

Source: Chenje, Sola and Paleczny, 1998.

Table 6 shows the number of farming units and distribution patterns of agricultural land per farming subsector in each NR prior to the agrarian reform. In 1999, commercial farmers occupied about 12 million ha, communal farmers 16 million ha, resettlement farmers 3.6 million ha, small-scale commercial farmers 1.4 million ha and state farms 0.1 million ha. The smallholder subsector consists of the communal, resettlement and small-scale commercial farmers.

The large-scale farms were located primarily in the areas of high agricultural and economic potential, in NRs I, II and III. One and a half million farming households in the communal lands farmed on about 49 percent of the country's agricultural land, of which more than 70 percent was in NRs IV and V. Thus, most of the communal lands are in the marginal agro-ecological regions. These are characterized by: (i) low rainfall, averaging 400-500 mm/year; (ii) severe dry spells in the rainy season; and (iii) shallow soils of low fertility. Such conditions are very marginal for the production of the major crops, even for drought-resistant grain crops such as sorghum and millets.

TABLE 6
Major features of farming subsectors up to 1999

Item

Unit

Small-scale farms

Large-scale farms

Communal land

Resettlement area

Small-scale commercial

Private commercial

State

Farms/households

Thousands

1 500

56.8

8.5

4.8

0.06

Total land area

Million ha

16.34

3.29

1.38

10.74

0.42

Share of total agricultural land

%

50.8

10.2

4.3

33.4

1.3

Average farm size

ha

18

58

162

2 223

7 644

Average arable land size

ha

3-5

3-5

10-40

Highly varied

NRs I & Ii

% of land

9

19

19

35

4

NR III

% of land

17

38

35

22

32

NRs IV & V

% of land

74

43

46

43

64

Irrigated area

'000 ha


7.2

3.6

126

13.5

National woodland area

%



21

44

35

Estimated population

Thousands

5 327

421

166

1 160

38

Population density

Persons/m2

32.6

12.8

12.0

10.8

9.0

Cropping intensity

% planted area of total area

14.0

5.8

4.3

4.2

2.3

Stocking rates

ha/LU

5.5

8.2

6.4


9.3

TABLE 7
A1 and A2 farming units created from acquired large-scale commercial farms, 2003

Province

A1

A2

A1

A2

Farms
(no.)

Area
('000 ha)

Farms
(no.)

Area
('000 ha)

% of area

% of area

Manicaland

227

181

140

76

70.5

29.5

Mashonaland Central

344

382

295

200

65.6

34.4

Mashonaland East

358

291

350

251

60.9

39.1

Mashonaland West

573

684

424

452

56.4

43.6

Matebeleland South

246

846

65

187

81.9

18.1

Total

1 748

2 384

1 274

1 166



Source: Government of Zimbabwe, 2003.

In the 1999/2000 season, the Government embarked on its agrarian reform programme. This entailed redistribution of land from the commercial farming subsector to new farmers. The Government moved to acquire 12.4 million ha of the 16 million ha in large-scale agriculture. This land came from 6 796 large-scale farms. Two new categories of farming subsectors were created, namely A1 and A2 farmers. A total of 127 192 households were settled under the A1 model, which consisted of demarcated villages with each household allocated five arable hectares and with communal grazing. The A2 model was based on self-contained farming units. A total of 12 943 individuals were allocated A2 model farms. Table 7 shows the number of farming units under each model per province as at March 2003.

In December 2000, the Government published Structural Instrument No. 288, which prescribed maximum farm sizes for all the NRs (Table 8).

TABLE 8
Farm classification and maximum farm size following the 2000 land/agrarian reform

Natural Region

Small-scale commercial farms

Medium-scale commercial farms

Large-scale commercial farms

Peri-urban commercial farms

(ha maximum)

I

15-25

100

250


IIA

25-40

200

350


IIB

40-50

250

400

15-50

III

60-80

300

500


IV

150-200

700

1 500


V

250-350

1 500

2 000


Source: MLARS, 2000.

Landholding, land use and cropping patterns in communal lands

Rainfall is the major determinant of the agricultural production patterns in Zimbabwe. Most crops are planted in November/December at the beginning of the rains and harvested between April and June. Winter wheat, barley and various horticultural products are grown in the dry season under irrigation. Irrigation schemes are also important in supplementing the production of wheat, tobacco, maize, cotton, soybeans, groundnuts and coffee.

The proportion of land allocated to food crops varies with the AEZ, availability or size of land, and farm productivity. In general, farm households in NRs II and III allocate 40-50 percent of the arable land under cultivation to food crops. The proportion rises to 60-70 percent in NRs IV and V.

Cropping patterns and land allocation to various crops within the communal area subsector by NR suggest the following salient features (Ashworth, 1990; Roth, 1990; Masters, 1991; National Early Warning, AGRITEX, 1994; MLAWD, 1993):

A comparative analysis of statistics on land allocated to each crop for the period 1980-1994 (National Early Warning Unit, AGRITEX, 1994) suggests:


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