Country Pasture/Forage Resource Profiles

Viet Nam

by

Dr. Nguyen Thi Mui

1. Introduction

2. Soils and Topography

3. Climate and Agro-ecological Zones

4. Ruminant Livestock Production Systems

Feeding systems and integration of livestock into farming systems

Grazing systems

Production constraints

5. The Pasture Resource

Natural resources

Improved pastures

6. Opportunities for Improvement of Fodder Resources

Practical applications of improved pasture in farmimg systems

7. Organizations and Personnel Involved in Pasture Research

8. References

9. Contacts

Viet Nam stretches 1,600 kilometres from China to the Gulf of Thailand, encompassing virgin forests, rugged mountains and fertile valleys. Shaped like an elongated S, or to the more imaginative a "descending dragon", Viet Nam covers the length of the Indochinese peninsula, bordering the China Sea in the East, Laos and China in the north, and Cambodia in the west (see Figure 1). Viet Nam’s territory includes a vast sea area including a large continental shelf and various islands. Viet Nam is endowed with considerable diversity and is located between 8⁰ 33' and 23⁰ 20' North and 102⁰ and 109⁰ 27' East. At either end of the country are two alluvial plains, the Red River Delta in the north and the Mekong Delta in the south.

Figure 1. Map of Viet Nam.
[Source: World Factbook]

Viet Nam has a history of 9,000 years. The capital is Hanoi and there are big cities such as Haiphong and Halong in the North and Ho Chi Minh, Danang, Hue, Nhatrang, and Cantho in the South. Although Viet Nam has 60 different ethnic groups and languages, Viet Namese is used throughout the country. According to the World Factbook the July 2006 population was 84,402,966 with a growth rate of 1.02%. There are a number of administrative units at province, district, city, town and commune level. Table 1 shows the extent of various land-cover types. Specific classes like marsh and mangrove are mainly in the Mekong Delta; forest is categorized as evergreen or deciduous; other groups like scrubland, agricultural area and water bodies are also noted.

i) Evergreen Forest is multi-level with an undergrowth of shrubs and natural regeneration. Trees of Dipterocarpaceae often dominate the upper storey, sometimes reaching considerable heights. Other families represented in the upper storey are Ebenaceae, Leguminosae, Guttiferae and Meliaceae.

ii) Deciduous Forests are dominated by species of Lagerstroemia and constitute a transition between closed evergreen forest and woodlands. Bamboos are the undergrowth of deciduous formations and also invade abandoned farmland.

iii) Mangrove occupies large areas in the extreme south near Ho Chi Minh City and small patches in the Red River delta. Species of the genera Rhizophora and Bruguiera account for three quarters of well-developed-stands.

iv) Marshes are in areas more or less permanently covered by fresh water. The following species occur: Eugenia elaeocarpus, Sterculia, Adina cordifolia, Calophyllum inophyllum as well as numerous species of palm. Homogeneous stands of Melaleuca leucadendron form behind the mangroves in areas not reached by brackish water.

v) Scrubland normally follows forest destruction, an open shrubby vegetation develops with sporadic distribution of trees with grasses on the ground.

vi) Agriculture is cultivated land and consist mainly of paddy fields, either irrigated or rainfed. It includes abandoned fields and exposed soil during the dry period.

vii) Water is lakes, rivers and water-filled depressions on the alluvial plains.

viii) No Data Available designates those covered by clouds and some topographic effects such as mountain shadow (as the information was derived from satellite imagery).

At constant 1994 prices, Gross Domestic Production (GDP) increased by 8.71 percent in 1995. In comparison with the index of 1995 (1995=100), GDP increased 40 percent in 2000. From 1995 all sectors of the economy continued to grow. Agriculture, forestry and fishing were 24.3 percent of GDP in 2000 (General Statistics, 2000). Gross output of agriculture in 2000 was 125,384.3 billion dong (1 US$ =15,000 Dong); crops had the highest share with 77 percent, livestock was 20 percent and services 3 percent.

The two major classifications of land are alienable (tenured land and farm land) and forest lands, both of which are lands of the public domain. Forest land covers 9,280,230 hectares of which 1,471,400 hectares are planted. There are types of forest classified as public forest, permanent forest or forest reserves, timber land, grazing lands and others and which are not alienated.

Total area of crops was 12,470,700 hectares in 2000 including cereals, annual industrial crops, perennial industrial crops and fruit. About 83 percent of farm land is used for annual crops and only 17 percent for permanent crops. Planted area and gross output of cereals (paddy and maize) in 2000 were 8,368,900 hectares and 34,483,500 tons, respectively. Data show a total area of 7,540,900 hectares of paddy and an output of 32,554,000 tons. All paddy is based on smallholders and is irrigated. Gross output of cereals per capita was:

Average farm area was 0.82 hectares, with close to 50 percent of farms below 0.50 hectares. Land areas and yield of crops and crop categories are shown in Tables 2 and 3.

Farm work is done by the farmers themselves with some help from their families or between families. In larger enterprises in the Mekong River Delta, farmers may hire other persons for field preparation, planting and harvest. Management of farms is in the hands of the family members. Payments to labourers are in cash or in kind depending on the prevailing rate in the locality. The labour required for different agricultural activities or for certain crops varies with location and cropping systems; the use of animals, tractors or machines facilitate work.

For the livestock sector, from 1994 to 2000, the average increase in cattle numbers was 2.1 percent, 6 percent for goats and sheep, 4.4 percent for pigs and 6.6 percent for poultry. The ruminant population has been increasing for the last six years, except for buffaloes which recorded a 0.43 percent reduction and although there was no change in the horse population between 1994 and 2000 there was a decline thereafter. Viet Namese statistics on animal numbers are given in Table 4.

Of the country’s land area, forest has the highest share with 28.6 percent. Agricultural land has about 18.7 percent while land for special use (hospitals, schools and universities, industry, mining and quarrying) and homesteads (fisheries, settlements and open land) account for 4.7 and 1.3 percent, respectively. At present, grazing areas are on community forest lands.

In terms of value of production at current prices cattle, buffaloes and small ruminants contributed 11,919.7 billion dong or around 65 percent of the total animal production in 2000. Poultry contributed 3,295.7 billion (18 percent), while non-meat production contributed just over 15 percent (2,802 billion dong). Livestock is a major source of income for smallholders. Production data are given in Table 4. Due to shortage of local milk, 90 percent of the country’s milk requirement is imported, largely in dry form (see Table 4).

Viet Nam can be divided into four physiographic regions: the Annamese extending from north to south through west-central Viet Nam, the Red River delta in the north, the Mekong River delta in the south, and the coastal plain in the east. The extremely rugged and densely forested Cordillera, a southward extension of the Yunnan Plateau, covers about two-thirds of the country. Parallel northwest-southeast ranges with several peaks rising to more than 1,800 metres dominate the northern half, and a series of heavily eroded longitudinal plateaus average elevation 750 to 1,500 metres extend into the southern half.

Figure 2. Soil map of Viet Nam
Adopted from FAO World Soil Map by R.H. Howeler
[Click to view full picture]

Viet Nam has fourteen soil groups and 31 soil units (a simplified soil map is shown in Figure 2), however, for easier evaluation these soils can be grouped into 2 big combinations:

Mountainous and hilly soils: most are Acrisoils, Ferralsols, or Alisols. Under annual cropping, without reasonable improving measures, the soil is rapidly degraded. The mountainous and hilly soils should be reserved for afforestation, cultivation of perennial crops, and fruit crops with appropriate protection measures.

Delta Soils. The centres of food production are mainly the deltas of the Red River, the Mekong River and other rivers. These are regions with high levels of intensive cultivation and crop intensity. With irrigation, moisture is sufficient, the rate of soil degradation is low; alluvial deposits bring fertility annually; this is often augmented by organic and mineral fertilizers.

The soil and vegetation characteristics of the main agro-ecological regions are described below:

The topography slopes from Northwest to Southeast with an average altitude from 400-500 metres. In coastal regions bordering upon the deltas, there are sloping hills and land with an altitude above 200 metres. Soil developed on calcareous low hilly and mountainous regions belongs to the yellow and red group. Alluvial soils are found in the valleys, along rivers and deltas. Two thirds of the forest has been removed and bare hills remain, or a thin secondary forest cover which can regrow in areas of high rainfall. Highland soils are easily lost through erosion.

This region and the Northeast are bordered by a range running from Nag Son and Coc Xo to Tam Dao. The border with the Northwest is the Hoang Lien Son range. Bare hills, and mountains cover 3,300,000 hectares. The main geomorphological units are

• High mountains (above 2,000 metres) are strongly dissected; deforestation has brought about increasingly serious erosion.
• Low hills and mountains (under 1,000 metres).
• Highlands and calcareous mountains remain in Dong Van (1,600), and Quan Ba (1,100 m- 1,200 metres).
• Valleys and swamps are found mainly in the south of the area. Although their area is not very large, they play an important role in agriculture.

The soil developed on low calcareous hills belongs to the yellow and red group. Alluvial soils are found in the valleys along rivers and deltas. Two thirds of the forest has been removed and bare hills remain; a thin secondary forest cover can regrow in areas of high rainfall. On highland areas soils are easily lost through erosion.

The land slopes from northwest-east south, bounded by the Hoang Lien Son range and Pulasan-Pudendinh and Panamas ranges along the Viet-Lao border. Mountain ranges and highlands are divided by valleys, large rivers and streams running North West-Southeast. This region can be divided into geomorphic forms as follows:

• High mountains (over 2,000 metres) in the northwest are strongly eroded, ending in the Hoang Lien Son range and Puxilung block.
• Average mountains (1,000 - 2,000 metres), these are also strongly eroded.
• Low mountains (under 1,000 metres) are strongly eroded, their average altitudes are from 400 metres to 800 metres.

The soils of the region are: yellow-red, yellow-red humus group on the mountains and humus soil on high mountains. The soils on the level land are alluvial, black, deposited soil, brown soil on neutral and volcanic rocks, and red-brown soil on calcareous rocks. In general, soils are acid and poor, and very shallow. On the calcareous highlands and Dien Bien and Pudendinh regions, the soils are relatively deep.

Average mountain height is 1,000 -2,000 metres : these mountains form a narrow range along the Viet-Lao border, including some with altitudes above 1,000 metres and some are above 2,000 metres. However, hills under 1,000 metres account for much of the region.

The main soil groups in the mountains are yellow-red, with humus soil. The main soil group of low hills is yellow-red soil on sedimentary rocks. In the delta the soils are alluvial coastal soil and coastal sand soil.

Central Southern Coastal Region

The Central southern coastal region consists of Bach Ma and the South-eastern Nam Truong Son ranges, which account for a large area. Deltas cover small areas. The arc-shaped mountains make up adjoining ranges with their branches stretching to the sea.

Above 1,000 metres the main groups of soil are: yellow-red humus and humus soil while below 1,000 metres the main soil belongs to the yellow-red group. Nam Ngai delta has the highest amount of alluvium in Quang Nam and Quang Ngai provinces.

Except on mountains, most soil is alluvial from the Red and Peace rivers. Alluvial land on river banks is extended by about 13,000 hectares by annual silt deposits, of which 74 percent is from the Red river and of light mechanical composition, fertile, suitable for industrial trees, food crops and food trees. Alluvial soil covers the highest areas within dykes. On lower minor areas, swampy soil covers about 46,000 hectares. In coastal regions there is alkaline soil. Around the margin of the delta, there is infertile, eroded grey soil which has been cultivated for a long time.

Tay Nguyen Region

Tay Nguyen, at average altitudes of 500 to 600 metres, is mainly on Bazan red soil, calcareous rocks and granite hills. Dac Lac highland is lower than Gia Lai highland, and average altitudes are 400 metres to 500 metres.

In the South, on the Di Linh and Bao Loc highlands, the main soils are brown ferralitic red soil generated from Bazan rock, with 10-12 metres thick, black, colour faded grey soil, yellow-red ferallitic soil on the sediment rocks and alluvial soil deposited by rivers and streams.

There are two main soil groups. Grey soil covers 34.26 percent of the region. Yellow red soil covers 44 percent. The yellow-red soil group of red-basalt soil generated on basalt rocks, is heavy with a, high silt and humus content.

The Mekong delta, a major area of food production, is alluvial and of low relief.

Its latitude range means that Viet Nam has a tropical monsoonal climate with hot winters in the south and cool winters in the north. The main climatic zones and number of wet and dry months are shown in the agro-climatic map in Figure 3. Nine agro-ecological zones are recognized which are described briefly below (and see Figure 4):

Figure 3. Viet Nam: The main agro-climatic zones
Adopted from Agro-climatic map of S.E. Asia
Source: Huke, 1982
[Click to view full picture]

North-eastern Region

The Northeast suffers most from the effects of the Northeast monsoon. The cold season comes earlier than in other provinces. Winter temperatures are from 1 to 10 ^oC lower than other regions. Average January temperature in Cao Bang is 11.5 ^oC and in July 26-27.7 ^oC; in Quang Ninh in January is 15 to 16 ^oC and in July 47- 28.8 ^oC. The rainy season starts between May and September and its duration can vary from 4 to 10 months with the yearly rainfall more than 1,276 mm, except for coastal regions. The number of rainy days reaches 120-160. This supplies enough moisture for 7 to 9 months.

At altitudes of 500-600 metres, trees remain of walnut, Pines such as Pinus caribaea, Pinus khasya, Pinus dalatensis, green ironwood Cephalotaxus mannii, Cephalotaxus oliveri, Amentotaxus argotaenia, Manglietia chevalierii, Manglietia conifera, Manglietia insigni, Vatica cinerea, Vatica mangachapoi, Parashorea chinensis which can grow in the cold and dry climate. These trees also remain in minor forests.

Figure 4. Viet Nam: the nine agro-ecological zones
[Click to view full picture]

In the mountains, the monthly average temperature is over 20 ^oC from March to November. The highest monthly temperature is hardly above 28 ^oC, but night temperature in some places falls to below 1 ^oC. In high mountains, the winter is cold and it can freeze with snow and hoar-frost; average temperature exceeds 20 ^oC from July onwards. Winter lasts from 70-100 days. The average day temperature is 15 ^oC. The average number of days below 10 ^oC is 50.

This region is moist throughout the year, with much heavy rain, and the highest rainfall in the country. Rainfall in the less rainy season is 30-40 mm to 60-70 mm/month. By the end of winter, drizzling rains increase strongly. The number of drizzle days exceeds 50-70. The highest rainfall reaches 3,000 mm. In heavy rain centres the amount of rainfall reaches 1,500 mm/month but in drier years, does not exceed 1,500 mm/year. In the mountains rainfall is over 200 mm/month, lasting for 5 months constantly. In low hills and mountains the growing season is under 8 months and rainfall is from 1000-1100 mm/year.

Cattle and buffaloes have a long tradition. There are many precious forest trees such as Hopea recopei, Shorea henryana, and Vatica cinerea.

Due to the geographical structure, the winter is cold, with hoarfrost on high belts. In the summer there is hot wind. During winter the diurnal temperature range is 12 ^oC to 14 ^oC. Summer comes sooner than to other regions, from March night temperatures are over 30 ^oC, and the weather in April is really hot. The month with the highest average temperature is June, but in Lai Chau it is August, in Moc Chau, it is July. The maximum temperature measured is from 41.1 to 42.5 ^oC. The minimum temperature is from - 0.8 ^oC to 3.9 ^oC. The valleys are sheltered from wind, so the dry seasons are longer, and the yearly amount of rainfall decreases. Dry seasons last from 4 to 5 months. The rainfall is usually under 1,500 mm.

The varied climate and terrain has created a variety of forest forms. In the North and South East, there is evergreen, tropical-humid forest. The main families are Lauraceae, Fagaceae, Magnoliaceae, Araliaceae and Euphorbiaceae. These forests are characteristic of the ecology of the North-western region and cover a large area; they are also found in Hoang Lien Son on a much smaller area.

The East and Southeast of the region have a sparse tropical forest. On high belts, under 700 metres, forests are evergreen-wet and tropical. Trees include Dipterocarpus costatus, Dipterocarpus intricatus, Dipterocarpus kerrii, Vatica fleuryana, Vatica astrotricha, Hopea chinensis, Neohouzeaua. On low lands there is a type of deciduous forest, able to withstand wet and dry climate; broad leaved trees grow among conifers such as Keteleeria davidiana, Pinus khasya, Pinus mercusia and Podocarpus fleurgi. Under 700 metres trees are mainly Dipterocarpaceae, Vatica fleuryana, Vatica astrotricha.

Winters are cold, the average temperature in December to February is below 20 ^oC (about 16 ^oC to 19 ^oC). Average temperatures in July are from 28 ^oC to 29 ^oC. In January average temperatures of the North are from 16.5 ^oC to 17.5 ^oC and of the South from 17 ^oC to 20 ^oC.

There is much rain, distributed unevenly. This region suffers from violent storms, hot winds and a winter monsoon. The number of sunshine hours is from 1,500 to 1,700/ year. Calculated radiation is from 105 kcl to 130 kcl/cm²/ year. The yearly average rainfall of Tay Hieu is 1,268 mm, of the North it is 2,399 mm, and of the South is 1,300 mm.

In the North and Northwest the flora is partially isolated, deciduous, wet forests with: Combretaceae, Lythraceae, Meliaceae, Sapindaceae, Sterculiaceae and Leguminoseae. In the West above 700 metres, the flora is evergreen and isolated rain forests with Dipterocarpus costatus, Dipterocarpus intricatus, Dipterocarpus kerrii, Symplocos olivacea. On low land along the coast, uncultivated land accounts for approximately 1,400,000 hectares in which there are 85,000 hectares of planted forests and 300,000 hectares of bamboo.

The yearly average temperature is above 25 ^oC. There is no cold winter. The rainy season lasts from September to December or January. Above Quy Nhon, the average temperature is above 23 ⁰C; the yearly temperature range of the North is about 5 ^oC, of the South from Nha Trang it is about 3 ^oC. In the North (Quang Nam, Quang Ngai), there is heavy rain with 1,600-4,000 mm/year. In the South (from Binh Dinh to Ninh Thuan) rainfall only reaches 1,300 to 1,400 mm/year. Phan Rang is a dry area, the yearly rainfall is from 700-800 mm.

The flora of this region belongs to the hot and dry climate of the low mountain belt. Because the dry season lasts for 3-6 months it has a special flora with large isolated bushes and hard leaves. In the East, along central coastal regions, there are also plantations; the main trees are Pinus patula, Pinus caribaea and Eucalyptus. Coastal deltas are used for crop production. Main limitations: violent storms, hot wind, droughts and floods damage the region.

Every year there are about 60 to 80 days below 15 ^oC and there is hot wind during 38 days. Rainfalls of over 50 mm occur 7-12 times. The amount of moisture is enough for over 10 months every year. Radiation is abundant, 105l-120 kcal/cm²/year. Photosynthetic radiation is also high, 56-62 kcal/cm²/year. Rainfall is 1,600-22,00 mm/year. Sunlight is from 1,600 to 1,800 hours/year.

Annual average temperatures are from 21 ^oC to 23 ^oC. The hottest months are March and April, the coldest is January. Minimum night temperature are from 5 ^oC to 8 ^oC in Da Lat and some time it can be below 0 ^oC. The diurnal temperature ranges are from 8 ^oC to 10 ^oC.

Moisture is insufficient from December to March. In many places it rains continuously for five months with more than 200 mm/month (from May to September). Cheo Reo has rainfall of more than 200 mm for two months but yearly amounts are from 1,200 to 1,800 mm and in Buon Ma Thuat it is no more than 1,400 mm.

The flora belongs to the isolated and sub-tropical forests of the highland and mountainous region and consists, according to the altitude, of the following floristic types. Above 1,000 metres there is a highland climate, so there are isolated sub-tropical forests with Pinus patula and Pinus dalatensis. Main planted trees are pines, Pinus massoniana, Pinus khasya, Pinus dalatensis, Amentotaxus argotaenia, Amentotaxus poilanei, and tea. Below 1,000 metres, there is tropical, dry broadleaf forest with bushes and tall tropical grass. Main plants are: Cephalotaxus mannii, Amentotaxus yunnanensis, Manglietia chevalierii, Shorea guiso, Parashorea chinensis, Madhuca alpina, Madhuca firma Keteleeria davidiana, Pinus khasya, Pinus mercusia, Podocarpus fleurgi, and other families such as Lauraceae, Fagaceae, Magnoliaceae, Araliaceae and Euphorbiaceae.

The yearly average temperature in the mountains is 21 ^oC. The winter diurnal temperature range (from November to April) is 10-14 ^oC and of the other months from 7 ^oC to 9 ^oC. In high and average mountains there is not enough moisture for the whole year; in low mountains and deltas, moisture is just enough for nine months - usually 7-8 months have above 100 mm/month and there is more than 200 mm for six consecutive months. The months, with the highest rainfall are July and August. Rainfall in the mountain is 1,100 to 1,200 mm/year and in the delta from 1,400 to 1,600 mm. The driest months are November and December. Yearly sunlight hours exceed 2000. January, February and March all have more than 200 hours/ month. September has the lowest sunlight time, 100-120 hours.

Annual average temperatures are from 26-27 ^oC. In Can Tho, the maximum night temperature is 40 ^oC and the minimum night temperature is 14.8 ^oC. The amount of rainfall in the west is very variable with eight months receiving more than 100 mm among which there are six, consecutive months with 200 mm/ month. In Ca Mau it rains continuously for five months with 300 mm/month. In the East and the Northeast of the deltas rainfall gradually decreases from more than 2,000 mm to 1,400-1,600 mm. In some places, during seven months, it rains continuously and for two months receives over 200 mm/month, such as in Chau Doc, Cao Lanh, My Tho, Ba Tri and Moc Hoa; the yearly rainfall is more than 1,500 mm. Sunlight hours are more than 2,700 in the Northeast and 2,300 hours in the west. April has more than 200 hours of sunlight.

The Mekong delta has violent floods in September and November. River levels rise at the end of September and the beginning of October and fall in November - then comes a dry season. In the floods, water covers a third of the delta; some places are flooded to 3-4 metres. In some places, salt water encroaches into the delta for 50 km. Salty lands (744,000 hectares) cover 18.9 percent of the region with high alluvium levels.

In Viet Nam ruminant production is based on small households; there are few dairy cattle in large commercial units. About 90 percent of farm households keep three to five cattle, mainly for draught, which can be sold when they need cash. There is some 10 percent of semi-commercial ruminant production units with 50 to 100 head in the North East, North West and North Central Coast; specialized cattle fattening is a source of main or additional income where crop production is not remunerative. Ruminant production is classified into dairy cattle, buffaloes and small ruminants.

See Table 5 for numbers.

Table 5. Population of dairy cows¹ and milk yield per lactation by years

Source: Vu Van Noi et al. (2002)
¹FAOSTAT data for numbers of cows are nearly double these figures.

Since 1958-1960 the Government has been developing milk production for improved human nutrition. The Roan White Black breed was imported from China and bulls of this breed were used for crossing with the Lai Sind in Bavi creating an F₁ herd. This F₁ herd could produce 1,800 kg/300 days of lactation. In 1970 to 1978, 1,500 Holstein Friesian were imported and raised in Mocchau, Sonla and Lamdong - milk production was 3,800-4,000 kg per 300 days.

From 1990-2001 dairy cattle numbers increased 3.8 times, and from 1999 to 2000 numbers rose from 30,000 to 40,000 and 42,000 in 2001, in which milking cows are around 18,000. At present 99 percent of dairy cattle are F₁ and F₂ Holstein Friesian (HF) in the structure of breeding (89 percent F₁ HF and 10 percent HF) and a few crossbred of F₁ Sindhi (1 percent ). From 1994 to 2001, milk yield per lactation of F₁, F₂ HF increased from 2,330 to 3,300 kg. For pure breed HF, milk yield increased from 3,300 to 3,850 kg per lactation.

Dairy cattle are kept in three regions: (i) Ho Chi Minh City and peri-urban areas (some 85 percent of dairy animals); (ii) Provinces in the North (13-14 percent), and (iii) Provinces in the Central region (about 1 percent). About 94.5 percent of dairy cattle are kept by small households with 3-5 head, there are some 0.5 percent of large farms with 50-100 head and another 5 percent are kept in large units to supply breeding stock for developing dairy cattle nationally. The total population is around 35,000 dairy cattle, mainly in peri-urban areas. Milk production was 45,000 tons in 1999, accounting for 10 percent of the country’s demand (7 litre/person/year), thus the bulk of the country’s milk requirement is imported (Vang, 2000). According to FAOSTAT (2005) milk production from cows tripled between 2000 and 2004 to nearly 150,000 tonnes

In Viet Nam dairy cattle production is part and parcel of a crop-animal system; an important feature is its rapid expansion in smallholder areas, driven essentially by urban demand, and the opportunity to generate income. Ownership of 2-15 animals and a small area with crops or pasture, leads to a situation in which milk production is a major component of farm income. This model is very common in peri-urban areas, where good markets and production services are found. The major constraints to production in these systems are availability of suitable animals, feed resources and improved feeding systems, improved breeding, reproduction and animal health care, management of animal manure, and organized marketing and marketing outlets. In spite of being mainly on small farms production has provided good income compared to other jobs. With stable milk price from year to year, a high net income from 5-20 percent in dairy cattle production is obtained by the farms (Table 6).

Table 6. Net income from dairy cattle on small scale farms

(*: 1 $ = 15,000 VN Dong)
Source: Vu Van Noi, 2002

The main source of fattening cattle is the local Vang breed which is small, average live weight about 140-160 kg/head for female and 250-280 kg for male, with a killing out percentage of about 42-44 percent. Pure Sindhi was imported in 1923; bulls of this breed crossed with Vang improve body weight of the F₁ female up to 35-40 percent and the carcase-weight by 44 to 49 percent. With the use of F₁ Sindhi female crossed with Charolais bull, F₁ can be 300 kg and carcase percentage of meat can be increased from 53 to 54 percent. Using F₁ Sindhi female could improve the beef herd not only by improving body weight but also to use as the source for continuing to cross with the male Holstein Friesian to improving body size. Cattle are mainly raised in hilly or mountainous areas. Beef cattle are raised on small farms with 2-5 head although there are some farms with 50-100 head. Some areas such as peri-urban Hanoi, Bienhoa, Ho Chi Minh City and large farms with many F₁ Sindhi females, cooperate with other regions to increase the size of beef cattle. The population of cattle by region from 1995 to 2000 were as shown in Table 7.

Table 7. Population of cattle including dairy cattle (‘000 head)

Source: General Statistics, 2000

Buffaloes are considered as a long-term investment by farmers and occupy a very high position as a source of inheritance from one generation to the next; Viet Namese farmers call buffaloes "the beginning of inheritance". In general, village farmers do not use the banks since they live in remote areas and, after all, do not have excess cash to deposit. What they earn in cash is barely sufficient for subsistence. Livestock is generally a means of saving: poultry and pigs are short term savings while buffalo and cattle are long term ones. In case of crop failure buffaloes or cattle will be sold to obtain cash. For traditional ceremonies such as marriage or some religious rites, farmers sell buffaloes or slaughter them for meat. Buffaloes are stronger than cattle and, in the deltas, can be used on both high and low land. Their value is measured in terms of draught power, amount of manure and partly meat. Draught power is not as critical as formerly, and since agricultural mechanization is developed in some regions the role of buffaloes is sometimes neglected. Even if soil preparation could be mechanized, the buffalo remains important for rural transport and meat. Buffalo meat accounts for half of all beef. Despite this the buffalo herd remains static; numbers fell by 0.43 percent from 1995 to 2000 (General Statistics, 2000) and have remained the same from 2000 to 2004.

Swamp buffalo rearing is a backyard activity with 99 percent in the hands of smallholders, mainly the rice farmers, for draught power. Each farmer keeps one or two buffaloes and maintains them by grazing on roadsides or common land. Only two state farms keep a few dozen to a hundred dairy buffaloes. In semi-intensive systems dairy buffaloes are raised mainly for milk and are stall fed; forage or grass are cut and carried. Rice straw and crop residues are supplementary feeds. Crop by-products are mixed with the concentrate. Occasionally buffaloes are given urea molasses blocks or urea treated rice straw. A very few herds larger than a dozen are kept in mountainous areas, where grazing land is still sufficient. All buffaloes are of the swamp type and small. Adult weight is 340 kg, and a new born calf is about 22-23 kg. After weaning at 6-12 months, calves grow slowly, but growth improves after 12 months. The body weight of calves at 12 months is 150 kg. There is a small herd of Murrah buffaloes, imported from India in the seventies, but its number has gradually declined. The outlook for dairy buffaloes in Viet Nam is not clear.

The major cause of low productivity of ruminant livestock, especially in hilly land, is lack and poor quality of feed. The main feeds are crop residues, permanent pastures and other agro-industrial by-products. Pasture area is declining steadily as the increasing human population demands more land for crops while there is a strong interest from farmers to maintain animal numbers because of the need for draught power.

Table 8. Population of buffaloes in Viet Nam by region (‘000 head)

Goat distribution is closely related to their owners’ traditions and ecological conditions (Tran and Nguyen, 1990). Most goats, (72.7 percent 25,000 head) are in the northern, mountainous provinces. They are also found in coastal regions of Central Viet Nam, where the climate is hot, dry and water is scarce (21.3 percent ). Only 6.3 percent are in South Viet Nam (Binh, 2002). Generally goats are raised in relatively dry areas with poor vegetation. In a harsh environment, goats perform better than other animals.

Approximately 95 percent of goats are local breeds: the main ones are Grass breed, Bach Thao and cross bred. The Grass breed is wide-spread in many ecological zones; they are well adapted to poor nutrition and management, small and well known for high prolificacy. Most goats are reared for meat. The Bach Thao is bigger than the Grass breed and also are dual-purpose for meat and milk; average milk yield varies from 1.5-3 litre/day over 150-165 days.

Since 1993 the demand for goat products (both milk and meat) has increased considerably but returns to farmers remain below potential due to low productivity, largely associated with feed quality. The Government places a high priority on the development of viable goat rearing; improving access by very poor communes to breeding schemes, and working with communes to improve husbandry and feeding strategies for goats are appropriate means of addressing rural poverty. Six breeds: Barbary, Beetal, Jumnapury, Alpine, Saanen and Boer were imported to improve body size and milk yield of local goats.

Most goats are privately-owned (Nguyen, 1988) by smallholders with an average of 5-7 animals. In forests, mountainous and hilly regions, many farms keep 100-200 goats. State farms just maintain some for research and breeding. Goats are kept in fields during the day, at night they are housed without feed or water. In the plains of North Viet Nam meat goats are herded, but in the South they are penned or tethered under fruit trees. Dairy goats are kept in pens with feed and water. The management of reproduction is poor. For meat goats, bucks and does run together without controlled mating which leads to high mortality of new-born kids. However, dairy goats are very well managed.

Feeding systems and integration of livestock into farming systems

Dairy production is most important in the South-eastern region, where feed can come from green fodder (native and cultivated grasses, legume forages), crop residues, agro-industrial by-products and concentrates (Table 9).

The limited amounts of good roughage, combined with intensive production in peri-urban areas has forced dairies into heavy dependence on concentrates; this has increased feed competition with other livestock. Better use of local resources by improving low quality roughage, better feed management and preserving high quality green fodder by improved storage methods are the most promising strategies for reducing feed costs and dependence on other feeds. Green maize is grown and supplied by a large number of farmers to feedlot operators and dairies. Fodder production has taken over a significant portion of the maize grain area. Some farmers prefer to grow fodder maize because they can solve the year-round green fodder supply for dairy cows, and especially in the dry season.

In the North Central and South Central Coast, where fattening of one or a few cattle is common, fresh grass, cane tops, maize stover, and rice straw are supplemented with fresh Leucaena leucocephala leaves. Some farmers feed a concentrate mixture at 0.5 percent of the animal’s body weight. Chopped leucaena or cassava leaves, are mixed with a home-mixed concentrate of maize, cassava meal, rice bran, salt, ground oyster shell and molasses.

In rice growing areas, weeds constitute about half of the feed (from road edges, fields and ponds) with rice straw and other crop residues. Animals are stall fed and tethered in uncropped and idle land during the growing period of the rice. Rice straw is the principal feed after harvest; other crop residues such as maize stover and legume hay are fed, when available, in the wet season. At rice harvest, paddy fields are communal grazing in the short gap between crops, which may be two or three times per year depending on the number of rice crops grown.

Rice straw, the most important feed, is readily available throughout the country, with a total 25-30 million tons produced annually (Bui Van Chinh and Le Viet Ly, 2001), of which part is burnt or left in the field, some is used for fuel or mixed with manure for fertilizer. Rice straw is low in available energy, protein and vitamins and imbalanced in essential minerals, but it contains a large pool of structural carbohydrates which can potentially be degraded by rumen microbes into volatile fatty acids, and thus an energy source for ruminants.

Urea treatment is the most suitable method of improving the quality of rice straw and increasing crude protein concentration and rumen degradability. A combined ration of green grass and Urea Treated Rice Straw (UTRS) increased degradation of organic matter, crude protein and crude fibre (Tuan, 2000). Replacement of grass by UTRS 50:50 for lactating cows in winter is as good as feeding grass alone in terms of milk yield, body weight gain and feed conversion (Mai Van Sanh et al., 2001). Treatment with urea (50g/kg DM rice straw) preserves fresh rice straw safely and improves its nutritional value. Urea-treated rice straw is a palatable roughage that can replace elephant grass in milking cows’ diets at high levels (75 percent), resulting in increased milk fat and without any effect on milk production (Man and Wiktorsson, 2001).

Cassava tops and Gliricidia can be ensiled by conventional methods, with or without additives. Ensiling reduces cyanogen content markedly by HCN volatilisation and to a lesser extent, the tannin content of the raw materials. A supplement of cassava top silage, especially with a molasses additive, to a grass diet of dairy heifers, increased the dry matter and digestible crude protein intake (Man and Wiktorsson, 2001).

Goats usually graze natural pasture or feed on leaves from trees. According to Nguyen (1972) a hectare of rocky mountain can keep 4-5 meat goats, and they can be raised on mountains with 28-52 percent of slope. In the plains goats graze on grass and leaves such as bananas, Sesbania, Jackfruit, Acacia and Cassava. Concentrates are not used for meat goats. The most important feed is grass from roadsides, fields and ponds. Crop residues are the main feed in the dry period, but their nutritive value is often below the level required for production. Dairy goats in hilly areas are commonly tethered and given supplements of high protein foliage which is bundled and suspended under the house or from trees. Plants used include Sesbania, Leucaena, Gliricidia sepium, Flemingia macrophyla as well as Jackfruit (Artocarpus heterophyllus) leaves. These are high in protein and ash (Nguyen Thi Mui et al., 2001ab).

Recent research has concentrated on increasing feed resources by growing crops with high yield, good nutritive value and good adaptation to hilly areas, especially in the dry season. Sugar cane and multi-purpose trees have proved to be particularly suitable. Pigs and young goats are fed sugar cane juice, the tops are fed to mature goats, peeled stems are used as a basal diet for rabbits and pressed sugar cane stalks are fed to buffaloes and cattle. Feeding systems based on sugar cane are being introduced to farmers in all hilly areas, where the intensity of land use is not high and there is a potential for growing more cane, provided a sufficiently attractive market for livestock products can be developed. Sugar cane has commonly been used as a feed for cattle in the dry season when the availability of conventional forages is limited. A model for using sugar cane as a feed for ruminants, for growth or milk production must take into account its high fibre, low protein and high energy content. Generally, when the level of sugar cane is 30 percent dry matter in the diet, there is a positive effect on both the liveweight gain of goats and milk production of cows (Nguyen Thi Mui et al., 2000). In sugar producing areas cane tops constitute 75 to 100 percent of the feed after the harvest and cane milling season which coincides with the dry season.

In most developing countries, crop-livestock production systems form the backbone of agriculture. Systems involve crops, livestock, land, water etc., in which these sub-systems and their synergistic interactions have a significant positive and greater total effect than the sum of their individual effects (Edwards et al., 1988). In Viet Nam these systems are called VAC systems and combine home gardens, fish ponds and livestock; they have been developed for a long time in many agro-ecological regions (Thien, 1998). Mixed systems account for the highest proportion of the meat producted in the country. Diversification, saving and recycling resources are their basic characteristics, which provide stability and a positive environmental impact. However, mixed farming systems bring more management complications, difficulties in isolating problems and generally lower yields compared to specialised and intensified ones. The feeding of animals in mixed crop-livestock farming systems revolves around the use of crop residues, weeds, tree leaves and planted fodders.

Before 1995 in hilly land, an area of forest after burning was used for crops such as maize, rainfed rice, and cassava. With no fertilizer use there was rapid exhaustion of soil nutrients. Areas could be used for 2 to 3 years then most remained fallow for 6 months to 1-2 years, even 10-12 years and were used for grazing volunteer vegetation. Cattle, buffaloes, goats and sheep grazed these fields until fertility recovered and farmers could have the next cycle of crops. Other sources of grazing were free in common areas or land around national forests, where feed was available. Since 1995 the forest is being divided for farmers according to Government policy. Grazing is limited to land very far from farm houses inducing a high risk.

In intensive farming there is little space to keep livestock and grow improved grasses. Farmers prefer small ruminants to cattle and buffalo; they keep livestock as savings: chickens and pigs are sold to meet daily needs, small ruminants are sold to meet seasonal needs (e.g. school fees, clothing); large ruminants are sold to meet occasional needs (e.g. weddings, building special houses). In intensive crop areas ruminants are kept for draught and saving and are always stall-fed. For improved forage, cut and carry is usual and forage is fed at night as a supplement. Under coconuts, oil-palm and rubber stall-feeding or tethering may be used.

Free grazing is only done on uncropped land, common land or fallow. In the high mountain areas of the North Northeast and North-Viet Hoang Lien Son there are two feeding systems (i) semi-intensive grazing and (ii) "feeding on the back". In the first farmers keep their stock at home and cut and carry is used during the rainy season when crops are growing. After harvest ruminants are allowed to graze the fields until the next crop and are housed at night. For the second, animals are penned all the time and farmers feed them during the day. Feed is collected from the field and forests; fodder shrubs and trees have been used to overcome feed shortage. In the North Central highlands where farmers keep big flocks (goats, sheep, cattle), animals graze forest land far from the houses. Children or a man always look after the grazing animals. At night animals are penned within a fence of Cactus, to protect them from wild animals.

Production constraints

The constraints associated with the growth and expansion of ruminant livestock production in Viet Nam are primarily:

• Dairy cattle have a long growing time and low coefficient of reproduction, and there is poor focus on genetic improvement, low knowledge about dairy production and herd management and no planning of breeding management from the government to the local level

• An insufficient number of high yield breeding stock; some provinces have brought breeds from abroad, this is only a temporary solution, and is not sustainable.

• Some areas with high potential for developing dairying such as Lamdong, Mocchau have no milk processing or marketing facilities,

• Lack of good quality feed and pasture, especially in the dry season or when drought occurs, because most farmers neither grow forage nor use the available fodder trees to supplement poor quality roughage. Shortages in feed are experienced due to inefficient use of farm by-products, and improper handling and processing of forage crops during peak supply periods or during harvesting of field crops.

• Lack of appreciation of the value of improved pasture. Only a few stock owners with over 20 dairy cows use improved pasture. Several have started introducing improved pastures on their properties but the forages are only in small patches that are generally left unattended or unprotected from free grazing animals. Expansion of improved pasture is very limited on land used for planting food crops or fruit trees. Improved pasture is based on wasteland, home garden, wild land, gravelly soil, low lying land or newly reclaimed land of too low productivity.

• The grazing system is not suitable for buffaloes and cattle since the size of the grazing areas is reduced day by day due to the conflict between buffalo, cattle production and the expansion of cropping and forestry.

• Unfavourable climate means a decline of one kilo of milk for each degree of temperature above 27 ^oC. Milk yield of Holsteins begins to fall above 21 ^oC, Brown Swiss drops at 24 ^oC and 27 ^oC for Jersey. Humidity promotes the multiplication of disease-causing organisms.

• Lack of credit for smallholders due to the large investment needed for financing milk cows and farmers must borrow with long term loans; lending procedures are very complicated and cumbersome.

The pasture area in Viet Nam is presented in Table 10. Total grassland is 534,100 hectares, or 5.7 percent of all cultivated land, which can be suitable for crops, trees, aquaculture and forestry. The productivity of grasslands has been adversely affected due to their small extent and overgrazing; at present they are producing about 20 percent of their potential because of poor management. In hilly areas natural grazing is still important for feeding cattle and buffaloes.

Depending on cropping patterns from region to region, pastures in Viet Nam are classified as:

In the high land, almost 70-80 percent of grasslands are covered with dominant species such as Digitaria adscendens, Panicum repens, Brachiaria dystachia, Brachiaria mutica, Chloris barbata, Cyperus rotundus, Cynodon dactylon, Axonopus compressus, Eragrostis nigra, Paspalum dilitatum and Panicum coloratum and shrubs or trees such as Artocapus heterophyllus, Hibiscus rosa-sinensis, Flemingia sp.

Several plants from rice and maize fields serve as forage, the majority them are weeds, and include Cynodon dactylon, Digitaria sp. and Dactyloctenium aegyptium. Other grasses used as feed are Imperata cylindrica, Paspalum conjugatum and Cyrtococcum sp. which grow naturally in orchards and wastelands or idle lots where most of the broadleaf species, such as Synedrella nodiflora, Pseudo-elephantopus spicatus and Asystasia gangetica, are also found.

In summer, most land is planted with rice, maize, groundnut, soybean and sweet potatoes. Forage from these crops provides the bulk of fodder for stall-feeding, especially for dairy cows. Urban cattle also feed on vegetable and fruit wastes. Community and government wastelands are used to some extent. Usually milking animals are stall-fed with green fodder and concentrates. Dry and draught animals are maintained on straw, maize stover, and community grazing lands. In winter all farmers sow green maize intercropped with vegetables. According to holding and herd size rice straw provides feed in winter. Other crop residues such as maize grain, maize stalk, cassava leaves, tubers, stalks and sugar cane tops, leaves or stalks are also components of livestock diets.

Since the mid nineteen-seventies, a dramatic shift in the paddy growing system took place, from single cropping to two or three crops annually. As a consequence, there is a serious shortage of space and forage for livestock. With the increased demand for milk, meat, and other dairy products, some farmers cultivate large areas of Elephant grass (Pennisetum purpureum), Brachiaria sp., Guinea grass and maize. Some farmers around such big cities as Ho Chi Minh City plant grass to sell green fodder to farmers raising dairy cows and forage cut-and-carry feeding plays a vital role for dairy goats, cattle and buffalo production. Every farmer allocates a piece of land for fodder crops in irrigated areas if they keep ruminants.

Several hundred improved tropical pasture accessions have been introduced and evaluated in different ecological environments over the last 20 years by the National Institute of Animal Husbandry (NIAH), and promising forages have been identified. Ruzi grass (Brachiaria ruziziensis), imported in 1991, grows well on grey-soil in the South East region and hilly land of the North of Viet Nam. The cutting cycle of Ruzi grass is quite good at regrowth 40 days with yields of 25 tons dry matter (DM) /ha/year (Duong Quoc Dung, 1995).

In high land with low fertility soil Panicum maximum Hamil, Panicum maximum Likoni, Pennisetum purpureum King grass, and Brachiaria mutica, have good production records, from 10- 23 tons dry matter/ha/years (Nguyen Ngoc et al., 1995). Other promising grasses including Guinea (Panicum maximum ) and Signal Grass (Brachiaria decumbens) which are able to perform in any of the sedentary and alluvial soils in all agro-climatic zones (Table 11). Brachiaria humidicola and Tripsacum andersonii (Guatemala grass) are important on acid sulphate soil and in areas with a high water table (Dung et al., 1999); on all soil, Napier (Pennisetum purpureum) is outstanding, Brachiaria ruziziensis, Panicum maximum TD58, Panicum maximum K280, and Panicum maximum Likoni have shown vigorous growth in acid soil.

In Daklak in the Central Highlands, some 21 improved grasses and legumes which grow well have been extended to farms rearing ruminants. All are planted for cut and carry but receive neither fertilizer nor irrigation; the edible biomass yields are promising (Table 12).