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Minerals Profile of Forages for Grazing Ruminants in Pakistan

Zafar Iqbal Khan Kafeel Ahmad Muhammad Danish Farhad Mirzaei
Vol 2(2), 74-91
DOI- http://dx.doi.org/10.5455/ijlr.20120407060608

The current research was carried out at Rakh Khaire Wala, well known as one of the most developed animal husbandry in Punjab, Pakistan. This location in the arid region, where sheep farming is a common practice, was selected for this study. The aim of the study was to determine and collect data on the mineral contents of forages or feedstuffs that are harvested and used in animal nutrition in the region, in order to gain information on the deficiency and/or excess of mineral levels for ruminants grazing therein, fed mainly with these feedstuffs. These pastures were visited twice during the study, in summer and winter, to collect samples in order to determine the effect of seasonal changes on the mineral contents of forages. In each location, samples from the available forages were collected. Forage samples were analyzed in order to determine the Ca, Mg, Na, K, Fe, Cu, Zn and Mn levels using an Atomic Absorption Spectrophotometer. These results show that pasture grasses/forages had sufficient levels of K, Ca, Mg, Mn and Zn to meet requirements of ruminant animals, but the occurrence of marginal to deficient supplies of Na, and Cu appear very likely. There is an urgent requirement for experimentation on supplementation regimes involving these minerals, so that appropriate recommendations can be formulated.


Keywords : Mineral Composition Forage Grazing Pakistan

Introduction

All the living systems require inorganic compounds and minerals for normal life sustaining processes. Furthermore, all animal tissues and feedstuffs contain minerals in widely varying amounts and proportions. Unlike other nutrients, minerals can not be synthesized by living organisms; therefore animals must acquire adequate amounts of required elements from their environment if survival and production goals are to be maintained. Livestock usually derive most of their dietary nutrients from the feed they eat, however, significant quantities of minerals may be obtained from water, soil consumption and feed contamination. Feed sources of minerals are typically divided into base feedstuffs (e.g. range or pasture plants, harvested forages, concentrates) and mineral supplements. Efforts to reduce the cost of mineral supplementation in livestock production require a thorough understanding of the supply and availability of mineral nutrients in typical feedstuffs (Dost et al., 1990).

Voluntary intake and mineral concentrations of base feedstuffs determines the level of mineral consumption. Adequate intake of forages by grazing animals is essential in meeting mineral requirements. Factors that reduce forage intake (e.g. low protein, high degree of lignification) also reduce total mineral consumption. The concentration of minerals in plants is dependent upon interactions among a number of factors including soil type, plant species, stage of maturity, dry matter yield, grazing management and climate (McDowell et al., 1983;Khan et al.,2005). Although total concentration of a mineral in a feedstuff is important, the biological availability of the mineral is equally important. Biological availability (absorption and utilization) of minerals varies substantially among animal species and breeds within a species, as well as among feedstuffs. The combination of all of these factors makes it extremely difficult for livestock producers to determine the actual mineral status of their herd, whether or not mineral supplementation is necessary and the degree of supplementation that may be needed to meet production goals (Dost, 1996, 1997, 2001).

Experiments have been previously conducted that address various aspects of mineral nutrition of grazing ruminants. Collectively these studies address seasonal/maturity changes in nutritive quality of native range/pasture plants in southwestern Punjab, Pakistan (Khan, 2003; Khan et al., 2005, 2006, 2007). The effect of forage intake on mineral bioavailability, and the effects of water stress, soil fertility, genotype and grazing management on forage chemical composition. The limiting factor in each of these experiments is the high cost of nutrient, particularly mineral, analyses.

In Pakistan as well as in Asian countries, malnutrition impairs livestock production. Pakistan’s overall livestock productivity is below average. Although large number of cattle, sheep and goats are found in Pakistan, the country produces only very small %age of Pakistan’s total meat and milk production respectively. Grazing animals in Pakistan subsist mainly on poor quality feedstuffs in the form of poor quality pastures in arid and semi-arid areas and hays and/or crop residues in the arable areas. In a few of the animal production centers where improved management is undertaken, the main supplements are energy and protein in the form of agro-industrial by-products such as cereal brans, molasses and oilseed cakes. Scant attention is given to the mineral content and nutritional balance of such diets. It has been widely established that available energy and protein of a feed are of prime importance to any animal but optimal performance is only possible if there is an adequate supply of minerals (McDowell, 1985; Khan et al., 2004). Seasonal variation affects livestock seasonal production in different regions of the world by affecting forage dry matter accumulation (Arizmendi-Maldonado et al. 2001a). Seasonal forage mineral nutrient contents stability may be achieved through successful breeding programs of forage plants (Mislevy et al., 1999). The primary source of nutrients and their transfer from soil to livestock in rangelands is forage. In Pakistan, ruminants rarely receive mineral supplements except occasionally common salt. Pastures are thus the main source of minerals, and only rarely can forages completely satisfy all mineral requirements of livestock (Miles and McDowell, 1983). Hence, it is important to know the mineral-nutrient concentrations of new varieties (McDowell 1992; Khan et al., 2006). Generally, Fe and Se concentrations increase as the seasonal forage yield increases (Espinoza et al., 1991; Santana and McDowell, 1994). In contrast Cu, Zn, and Mn contents were not affected by seasonal forage yield (Gomide et al. 1969; Santana and McDowell, 1994; Arizmendi-Maldonado et al. 2001b).

Due to increased demand, improved forage crops such as multi-cut oats, Trifolium, Medicago, Sorghum- Sudan grass hybrids, sorghum, maize and millet have been developed. These have become very popular in irrigated areas such as Kasur, Sheikhupura, Gujranwala, Faisalabad, Sargodha, Jhang and Leiah, and Renala Khurd (Punjab), Nowshera, Charsada, Mardan, and Peshawar (North West Frontier Province), and Hyderabad, Sukkur, Larkana, Halla, and Nawabshah in Sindh, for sale to peri-urban dairies. Therefore, this study was aimed at to evaluate the mineral composition of different forages both in natural pasture and improved varieties in relation to mineral requirement of ruminant in order to adopt various strategies for mineral supplementation for livestock at this semi arid region .This information on forage nutritive values would be useful for Pakistan as well as for other Asian countries with similar climate and ecological conditions.

Meterials and Methods

Samples of forages and grasses were collected twice from the Livestock experimental station in Punjab, Pakistan from different sites in the pastures of livestock’s farm situated away from 450 km southwest of Islamabad, the capital of Pakistan.(Fig.1) at Meteorological conditions described in Table1.All the samples were from the natural pastures and were obtained by pooling core samples from three positions within the pasture. The species collected included: Cynodon dactylon, Cynodon plectostachum, Pennisetum purporeum, Andropogon gayanus, Acacia brevispica and-Posopis cineraria, Lolium multiflorum, Sorghum sudanense, Pennisetum americanum, Vigna radiate, Panicum miliaceum, Vigna aconitofolia Paspalum conjugatum ,Drymaria cordata and improved pasture hay Medicago spp were taken as described above from stacks of forages at these sites harvested in June and August during summer and January and February during winter season, 2006.

Albizzia lebbek grown at the farm for grazing livestock in pasture of that specific site were harvested in February, 2006. Samples were taken by pooling leaves from mature trees. Leaves from the trees in the pastures were further separated into young and old. Pods with seeds on trees from the pasture were first air-dried and then separated into pods and seeds. Samples of Salvdora oleoides were taken in February, 2006 from a plain lower area at a Government research station in the pasture. The Prosopis spp samples were of the species mainly browsed by the browsing ruminants. Samples of forages remains were taken using the same procedures as for other forages. The forages residues were of natural pasture and improved varieties of forages grown therein, and most of them were being used in feeding experiments at Livestock experimental station.

Fig. 1. Location of experimental site at Rakh Khiare Wala near Leiah, Punjab, Pakistan.

 

Chemical Analysis

The dried samples were ground using a one-mm sieve and stored in plastic bottles ready for preparation. Samples were prepared for mineral analysis by the wet digestion method using concentrated sulphuric acid in presence of hydrogen peroxide. The concentrations of K, Na, Ca, Mg, Fe, Mn, Zn and Cu were determined by Atomic Absorption Spectrophotometer following the methods described by Mpofu et al.(1999) and Fick et al.(1979).

Statistical analysis

The data thus obtained during the study were analyzed by Statistical Analysis System (SAS,1987). Significance levels ranged from .05-0.001 statistical analyses .Differences between means were ranked using Duncan’s New Multiple Range Test (Duncan, 1955

Results and discussion

The total mineral content of feedstuffs is called ash. Forages normally contain 3 to 12% ash on a DM basis. Organic matter is determined by subtracting ash from 100. Minerals can be divided into two groups. Macro are those required by animals in relatively large amounts and include calcium, phosphorus, potassium, magnesium, sulphur, and salt (sodium chloride) while micro or trace minerals are required in small amounts and include iron, iodine, cobalt, copper, manganese, zinc, and selenium. It has been recommended that forages should be routinely tested for calcium and phosphorus. Other macro minerals, along with trace minerals, should be tested for once or twice per year to identify the imbalances in their concentrations (Clark et al., 1990). The analytical results for all forages and grasses as related to requirements of ruminants are presented in Tables 2-4.

Potassium

In this investigation the level of K in all the forages was above 8 g/kg recommended for grazing animals (Underwood, 1981). It has, however, been suggested that some ruminants with high producing, under stress such as heat stress, may require K level above 10 g/kg. Since only the residues of some forage crops approached this level (McDowell, 1985; Khan et al., 2005), it seems most unlikely that problems of K deficiency are likely to arise. It tended to be higher in some forage samples during this investigation. Similar K concentrations were also reported by Prabowo et al. (1990) in Indonesia, Ogebe et al., (1995) in Nigeria, and Tiffany et al., (2000, 2001) in North Florida. High potassium forages and low sodium chloride diets are seemingly contributing to reproductive losses in herbivores. Excessive potassium in forages induces deficiency of other minerals and immune suppression.  There appears to be a causal relationship between high potassium forages and a multitude of emerging opportunistic diseases of livestock.

In recent years it has become apparent that excessive potassium in the diet is a primary and significant cause of mineral antagonisms and induced imbalances in herbivores. This is certainly not a new discovery and it has been reported nearly 50 years ago, but potassium levels in forages have increased dramatically since that time and are continuing to increase (Dougherty et al., 1995). Environmental factors play an important role in potassium metabolism in plants. Potassium is naturally high in lush grass during the early grass-growing season especially when environmental conditions like high moisture and heat favor rapid grass growth.   Since potassium is the cation responsible for naturally protecting plants from droughts as well as from frost damage it is reasonable to assume that an increase in forage potassium may occur during and after frost damage to plants. To further complicate the cation imbalance, excess potassium antagonizes the uptake of sodium that has become naturally deficient in forages.  When herbivores consume these high potassium-low sodium forages, acute electrolyte and mineral imbalances may occur if they do not have readily available supplemental sodium chloride to counteract the high potassium in forages (Kakinuma, 1998).
Potassium in plants forms weak complexes and can substitute for similar cations, primarily sodium, and thus affect the sodium chloride or salt requirements for animals.  An excess of potassium, and a deficiency of sodium, may alter the balance of all other cations and anions.   Importantly, excess potassium can interfere with the uptake and availability of sodium, calcium and magnesium in the diet and may interfere with both magnesium and calcium metabolism.  When potassium spikes in forages, the anions chloride and sulfate may also increase which further exacerbates the imbalances of cations in forages.  An excess of chloride may influence calcium metabolism and cause excessive excretion and a calcium deficiency may occur. An excess of sulfates may interact with selenium and can cause a selenium deficiency (Islam et al., 2003; Bhatti,1996; Bhatti and Sartaji, 1996). Also, when there is a calcium deficiency, toxicosis from all minerals, essential and non-essential, is more likely to occur. The end result is cascading mineral imbalances, secondary toxicoses, and induced deficiencies of   essential trace and macro minerals.

When animals are exposed to high potassium forages, they display signs of salt deprivation and aggressively devour sodium chloride to counteract the excessive potassium in forages.  This may occur with any forage, but is especially common if herbivores consume rapidly growing lush grass and legumes. Also, it may occur if animals are fed hay high in potassium or if cattle are foraging corn stalks after the corn was heavily fertilized with either high potassium manure or high potassium fertilizers.  The salt deprivation behavior is especially apparent if herbivores are devoid of supplemental salt for only a short period of time (Baker et al., 1992).

In addition to grass, tetany which is commonly seen in cattle, other herbivores, including horses, sheep and goats exposed to high levels of potassium may suffer from a multitude of disease syndromes.  These include reproductive losses with abortions occurring during all stages of pregnancy, premature births, and weak offspring at birth. The high potassium may cause an antagonism to other minerals, and multiple mineral imbalances and induced deficiencies may occur. When this occurs, animals become susceptible to opportunistic diseases, which may also contribute to additional reproductive diseases of livestock. Potassium in different growing forages, is usually quite high (McDowell and Valle, 2000). Potassium levels of 0.6 to 0.8 percent of ration dry matter are considered adequate for cattle. In general, potassium levels of Ohio forages are adequate to excessive in potassium content. These high levels can be associated with reducing magnesium absorption and thus causing grass tetany problems. Therefore, always check potassium levels before any supplemental additions is recommended. Low concentrations of potassium have been observed in most of the forages during the winter (Clanton, 1980). Leaching during the winter may cause potassium levels in forages pasture to drop as low as 0.24-0.3 percent of dry matter during winter months (Sewell, 1990). Potassium can be supplemented to cattle in the forms of readily available diets such as potassium chloride, potassium bicarbonate, potassium sulfate, or potassium carbonate. If potassium is added for winter feeding, then it must be removed from the mixture when forages start growing in the spring. Growing forages are usually high in potassium. Thus, the grazing livestock consuming primarily a forage diet would receive adequate K. In certain regions of the world, it is possible that K deficiency could arise, in view of decreasing content of this mineral with increasing forage maturity (McDowell and Valle, 2000).

Iron

The forage contained Fe contents in   almost all the forages samples studied were above the levels of 50 mg/kg proposed as adequate for grazing animals (McDowell, 1985; Khan et al., 2005) Variations in the contents of Fe among grazing forages could be partly explained by forage species’ differences and the influence of grazing lands on the level of Fe in the soil. All the grazing pasture forages had higher levels of Fe than the critical content of Fe in animal tissues (30-50 mg kg-1 DM). Differences in the contents of Fe between the grazing different pastures forages and literature values could also be related by variations in the content of Fe in the soil, and climatic conditions between localities. Forage Fe content is a function of forage species, soil Fe content, nature and type of soil on which forages are grown (McDowell 1992; Serra et al., 1999). These forages had higher levels of Fe than the normal requirements of 30-60 mg Fe kg-1 DM of ruminants (McDowell, 1992). However, Fe bioavailability in ruminants would depend on feed mixture fed together and form of Fe in these feeds. Forage Fe levels during the study season were sufficient for the requirements of ruminants for optimal performance. These levels of forage Fe in the present study may support the reports of various researches, in Guatemala (Tejada et al., 1987) North Florida (Cuesta et al., 1993), Nicaragua (Velasquez-Pereira et al., 1997), and Indonesia (Prabowo et al., 1991). The generally high forage Fe found in this study is an agreement with the higher forage Fe value of 650 mg/kg reported by Khan (2003) in the similar region in Pakistan . According to Kabata-Pendiaus and Pendias (1992) the changing conditions of soil and climate as well as physiological state of plants affect the Fe absorption by the plants.

Manganese

High levels of manganese in forage can retard the growth of livestock. The feasibility of breeding for lower manganese concentration in shoots of various forages was examined growing in acid, manganiferous soil. Sampling leaves of a particular physiological age in a field-growing breeding population provided an adequate indicator of manganese concentrations in whole shoots. Forage Mn levels were above 40 mg/kg, the critical level and found to be sufficiently   higher to meet the requirements of ruminants. Similar levels of forage Mn   concentrations have already been reported in Nicaragua (Velasquez-Pereira et al., 1997), Indonesia (Prabowo et al., 1991) and in Guatemala (Tejada et al., 1987; Khan et el., 2007).

It has been reported that low soil Co level found in this ranch by Khan (2006) was also a possible explanation of high level of Mn in forage as these elements antagonize in the soil (McKenzie, 1975; Yan et al., 2006; Khan et al., 2007). On this ranch, mean forage Mn concentrations were although high but below the maximum tolerable levels (NRC, 1985). Most of the ruminants and particularly rams fed the least amount of manganese had low concentrations of manganese in heart and lung and a lower activity of manganese superoxide dismutase in heart than rams fed 45 8g Mn/g. The concentration of manganese in these tissues, and the activity of manganese superoxide dismutase in the heart increased linearly as the concentration of manganese in the forage consumed by these animals increased. An intake of 13 8g Mn/g of dry matter therefore caused some biochemical changes in rams, but was adequate for growth and wool production under the conditions of this experiment. Influence of manganese intake on body, wool and testicular growth of young rams and on the concentration of manganese and the activity of manganese enzymes in tissues is dependent on forage or diet Mn levels (Masters et al., 1988).

Sodium

The Na requirement for ruminants is often debated in the literature concerning the dietary concentration demand of the animals. An adequate range from 1-4 g/kg has been recommended by various researchers ( Underwood,1981; Little ,1987) .The present data show that with the exception of Albizzia lebbek, most of the forage samples examined were very poor sources of Na, such that routine supplementation is likely to be necessary. These values were deficient because of being lower than the critical values (requirement of ruminants) according to NRC (1985; Sial, 1991; Tudsri and Kaewkunya. 2002; Khan et al., 2007 ). This widespread deficiency in forage Na is corroborated with some earlier findings (McDowell et al., 1993), that the most prevalent mineral deficiencies for grazing animals in world were Na. In addition, deficiency of this element has been reported in many developing countries e.g. Nigeria (Gibe et al., 1995) and Colombia (Pastrana et al., 1991; Areghoere, 2002).

Sodium concentrations in forages were below the levels recommended for optimal animal productivity and production. Morris and Peterson (1975) suggested that a sodium intake of 0.87 g/kg was required to maintain an adequate Na and K ratio in the parotid saliva of ewe’s .Vincent et al. (1987) reported that milk production and lamb growth were unaffected by intakes, the ewes were in negative sodium balance. The content of Na in the ration is important in determining the adequacy of the minerals. To meet the need of highly productive animals, forage should contain more than 0.15% sodium (Committee on Mineral Nutrition, 1973). Na deficiency is more likely to occur in animal grazing tropical pasture species and these plants generally accumulate less Na than temperate species (Morris, 1980; Misrule et al., 2003). Natural forages low in Na has been reported in numerous tropical countries throughout the world (McDowell, 1985; Mutha and Pachauri, 2005).

Calcium

Forage Ca concentrations of 2-6 g/kg, with higher requirements for lactation have been variously recommended for cattle and sheep, Gill and Bhatti, 1996; NRC, 1985: ARC, 1980; Khan et al., 2006), the findings of Sykes and Field (1972) suggest that levels of 2.53.0 g/kg are adequate in most circumstances. Variations in the levels of Ca between findings in this study with values reported in the literature could be partly explained by different forage species, species composition, stage of maturity and season, and variations in soil characteristics due to location of the different grazing pastures at the ruminant ranch in this arid region of Punjab-Pakistan. Higher contents of Ca could probably be explained by proportion of forage species. Forages that were used in this study were harvested to include a mixture of grasses crop residues and legumes species that form the major portion of the diet consumed by grazing ruminants. In this region it could be assumed that legumes contain more minerals concentrations than would be in grass species, forage crop residues and legumes during winter seasons, which are richer in minerals, including Ca (Kim et al., 2006; Manson, 1990; Aregheore, 2002; Khan et al., 2007) than stem fractions of grasses (Underwood and Suttle, 1999). Mean forage Ca concentrations were adequate and sufficiently higher than the requirements of ruminants. Forage Ca requirements of grazing ruminants is a subject of considerable debate as the requirement is influenced by animal type and level of production, age and weight. Reuter and Robinson (1997) suggested Ca requirement for maintenance, growing and lactating sheep to be 1200-2600 mg/kg. Thus the forage Ca values found in this study was considered adequate for the optimum performance of ruminants. Similar forage Ca values as found in summer were reported by Pastrana et al. (1991a,b) in Colombia, Tiffany et al. (2000, 2001) in North Florida, Espinoza et al. (1991), in Central Florida and Cuesta et al. (1993) in North Florida. These results indicate that problems of Ca deficiency would not be expected.

Magnesium

The native and un improved pasture forages had lower levels of Mg than most species of forages and grasses However, differences in the content of Mg in this study with those in the literature could be partly explained by differences between forage species, level of Mg in the soil, influences of locality and climate, growth stage, proportion of leaf and stem fractions collected for mineral analysis, and season when forage sampling was done. The grazing pasture forages had slightly higher levels of Mg than the recommended requirement (ARC, 1980; Islam et al., 2003). These forages would therefore meet the theoretical requirement of Mg for beef cattle (NRC, 1996, Khan et al., 2007) and for lactating cows (1.2-2.1 g/ kg DM), Anonymous (2001). These forages had also higher levels of Mg than the recommended requirements for growing lambs and lactating ewes and goats (Meschy, 2000). The high forage Mg level in this study was above the requirement of ruminants suggested by Anonymous (1985). Similar values in winter forage Mg were reported by Salih et al., (1983), in Florida. Grass tetany is most common in lactating cows grazing lush spring pastures. During the early spring, climatic and soil conditions are cool and wet; plants will not contain adequate levels of phosphorus or magnesium (Khan et al., 2007). While both these minerals may be in adequate amounts in the soil, plant uptake is slow due to the cool, wet conditions. Fertilizing pastures with nitrogen and potassium is associated with increased incidence of grass tetany. Cows depend on a frequent supply of magnesium from the feed since mobilization of magnesium from the bone is not very efficient.

According to Dua and Care (1995), the dietary Mg availability to stock is markedly affected by other dietary components, especially K. High dietary levels of K and N will inhibit Mg absorption from the rumen. Ca and soluble carbohydrates may respectively increase and decrease dietary Mg requirements of livestock, whereas raised dietary P levels appears to lower the requirements for both Ca and Mg (Judson and McFarlane, 1998).

Zinc

It has been suggested that 30 mg/kg to be a critical level of dietary Zn, although it has been recommended that concentrations of 12-20 mg/kg are adequate for growing ruminants (ARC, 1980). The forages remains/residues may thus constitute a marginal supply of Zn the necessity for supplementary Zn needs to be kept under review particularly for goats and sheep in addition to cattle, which require some 35 mg Zn/kg diet (McDowell, 1978). The Zn content in these forages could be sufficient for recommended requirement for sheep. However, efficiency of Zn utilization of these forages would depend on zinc bioavailability, and its interaction with other mineral elements. Forage Zn concentration was also found above the requirements of ruminants during in winter (Reuter and Robinson, 1997). Almost similar results were reported by Prabowo et al. (1991) in South Sulawesi Indonesia and Tiffany et al. (2001) in North Florida. A number of factors including soil, plant species, pasture management, and climate, may affect the likelihood of Zn deficiency in ruminants. Cox (1973) reported the low level of Zn in soil and plants. Plant maturity has also been reported to affect Zn concentration of forage and it also depends upon the tissue type of plants (Underwood, 1981; Kabata-Pendias and Pendias, 1992).


Table 1. Meteorological conditions (Mean ±SD) recorded during the experimental periods

Winter Summer
Temperature 0C Relative humidity (%) THI Temperature 0C Relative humidity (%) THI
Day 11.8±2.9 67.9±19.5 53.7±4.6 Day 47.9±4.8 41.8±12.3 79.4±2.7
Night 6.8±3.9 85.6±13.7 44.6±6.3 Night 21.8±4.6 52.2±12.6 55.5±5.8

 

THI is the Temperature Humidity Index calculated as follows:

THI=04(dry-bulb thermometer temperature oF + Wet-bulb thermometer temperature oF)+15

 

Table 2. Mineral content of some dried leaves of different grasses from southwestern ranch in Punjab, Pakistan.

Forages
Description of dried leaves samples Macro minerals (g/Kg) Micro minerals (mg/Kg)
K Na Ca Mg Fe Mn Zn Cu
Wheat 20.50 0.70 3.40 2.30 712.00 217.00 48.00 6.40
Barley 15.70 0.60 5.30 1.90 894.00 215.00 41.00 6.80
Oats hay 16.40 0.17 1.80 1.65 265.00 106.00 35.00 7.00
Cynodon 21.30 2.13 5.87 2.15 421.00 219.00 38.00 8.80
Medicago 25.80 1.70 4.12 2.90 388.00 246.00 34.00 8.12
Trifolium 19.80 0.90 5.23 2.30 210.00 278.00 33.00 7.80
Mixed 15.40 0.80 5.34 2.17 608.00 334.00 45.00 8.30
Andropogon 27.90 1.67 2.13 1.80 850.00 48.00 27.00 4.20
Paspalum cojugatum 1.40 0.15 4.17 1.76 643.00 78.00 37.00 3.70
Cynodon plectostachchyum 1.20 0.06 2.42 1.80 912.00 67.00 36.00 6.30
Pennisetum purporeum 1.40 0.15 3.50 2.23 472.00 78.00 45.00 5.30

 

Table 3:- Mineral concentration of some forage residues from the farm in Punjab, Pakistan.

  Macro minerals (g/Kg) Micro minerals (mg/Kg)
Samples description K Na Ca Mg Fe Mn Zn Cu
Lolium multiforum 14.80 0.30 4.10 1.50 325.00 78.00 11.00 3.00
Sorghum Sudanese 10.70 0.50 4.60 1.40 117.50 90.00 12.00 5.00
Pennisetum americanum 11.70 0.30 4.30 1.90 170.00 59.00 26.00 6.50
Vigna radiate 17.70 0.40 3.90 1.80 196.00 191.00 17.00 14.00
Panicum miliaceum 10.70 0.60 7.70 2.20 103.00 71.00 24.00 14.00
Vigna aconitofolia 17.80 0/50 3.30 2.50 408.00 61.00 24.00 5.90

 

Table 4. Mineral content of Salvodora oleiodes, Albizzia lebek, and Prosopis cineraria at ruminant ranch.

Salvodora oleiodes
Description of dried leaves samples Macro minerals (g/Kg) Micro minerals (mg/Kg)
K Na Ca Mg Fe Mn Zn Cu
Young leaves 25.60 0.45 4.70 2.80 194.00 38.00 43.00 13.80
Old leaves 19.32 0.43 20.76 4.32 223.00 65.00 24.00 13.50
Small new branches 15.80 0.76 17.87 1.50 206.00 45.00 16.00 4.80
Fruits 17.70 0.54 4.80 2.34 154.00 34.00 49.00 14.67
Albizzia lebbek
Small twigs with leaves 15.00 1.80 23.3 3.50 244.00 155.00 52.00 11.40
Pods with seeds 23.80 1.80 8.50 1.90 114.00 48.00 35.00 7.60
Pods alone 15.70 1.70 15.50 1.40 592.00 58.00 42.00 7.80
Old and young leaves 17.20 1.80 31.76 5.40 295.00 445.00 66.00 7.90
Prosopis cineraria 19.70 1.25 8.90 3.60 188.00 154.00 53.00 7.50

 

Copper

It is commonly suggested that the dietary requirement of ruminants for Cu ranges from 8 to14 mg/kg (NRC, 1984; Khan et al., 2006). In this investigation the most of the forage samples analysed are only meeting the marginal to deficient requirements of this element. This situation may be even further complicated by high levels of dietary Fe which can be elevated by soil ingestion during grazing. Humpries et al. (1981) found that dietary concentrations exceeding 1 g Fe/kg can profoundly reduce the availability of ingested Cu; relatively slight and doubtless common levels of dietary soil contamination can produce Fe concentrations of this order (Healy, 1973; Khan et al, 2006), necessitating the serious consideration of providing supplementary Cu to the grazing livestock. Forage Cu content declines with forage maturity, and is higher in leaf vs. stem fractions (McDowell, 1996). Copper deficiencies in forages can cause poor reproduction, broken bones, weak calves, and light color hair. Discoloration normally occurs first around the eyes and tips of the ears. Sometimes, changes in hair color are not noted and the effect of a copper deficiency simply occurs as reproductive problems, scours, or calves older than four months ceasing to perform. Simmental and Charolais cows and their calves were more susceptible to copper deficiency than Angus cows fed the same diet (Ward et al., 1995).

It is worth mentioning that forage may contain an adequate level, however, if the diet contains either high levels of molybdenum (2 ppm) or sulphur (0.25%), both of these tie-up copper, rendering a deficiency. Ideally, the copper to molybdenum ratio should be around 5:1 (Munshower and Neuman, 1979). Legumes were blamed for increasing the molybdenum levels on reclaimed strip ground in Montana (Munshower and Neuman, 1979). High concentrations of iron (Phillippo et al., 1987) and zinc (Davis and Mertz, 1987) also reduce copper status and may increase copper requirements.

Conclusion

The minerals most widely present in inadequate amounts are Na, and Cu. It is stressed that data of the type presented here can provide only an indication of the existence of potential mineral deficiency problems, since animal selectivity usually results in the consumption of material of somewhat higher quality than that of the total available, and conclusive diagnosis must be based on the occurrence of a positive response to supplementary supply of the mineral in question. However, such data are vital in the formulation of critical supplementation experiments. There is an urgent need for appropriate experimentation so that soundly-based supplementation packages can be devised.

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Khan , Z. I., A. Hussain, M. Ashraf and L. R. McDowell. 2007. Assessment and comparison of blood plasma mineral concentrations of different classes of grazing sheep. Trace elements and electrolytes (Accepted).

Khan, Z. I. 2003. Effect of seasonal variation on the availability of macro-and micro, nutrients to animals (sheep and goats) through forage from soil. Ph.D Thesis Uni. Agric, Faisalabad, Pakistan. pp, 286.

Khan,Z.I, A. Hussain, M. Ashraf, L. R. McDowell .2006a.Mineral Status of Soils and Forages in Southwestern Punjab-Pakistan: Micro-minerals. Asian-Aust. J. Anim. Sci., 19: 1139.

Khan, Z. I.,   A. Hussain, M. Ashraf, E.E. Valeem, I. Javed.               2005. Evaluation of variation of soil and forage minerals in pasture in a semiarid region of Pakistan. Pakistan Journal of Botany, 37: 921-931.

Khan, Z. I, A. Hussain, M. Ashraf, M. Y. Ashraf, E. E. Valeem, and M. S. Ahmad. 2004a. Soil and forage (Trace elements) status of a grazing pasture in the semiarid region of Pakistan. Pakistan Journal of Botany, 36: 851-856.

Khan, Z. I.,   M. Ashraf, A. Hussain. H. W. Koyro, B. Huchzermeyer. 2005. Seasonal variation in the status of selenium in goats grazing native and improved pastures in a semiarid region of Pakistan. Deutsche Tierarztliche Worchenschrift , 112: 460-465.

Khan, Z. I., M. Ashraf, M. Y. Ashraf, A. Hussain, and L.R. McDowell. 2005b. Concentrations of minerals in milk of sheep and goats grazing similar pastures in a semiarid region of Pakistan. Small Ruminant Research. (in press)

Khan, Z. I., M. Ashraf and A. Hussain. 2006d. Evaluation of manganese status of grazing sheep in a semi-arid region of Pakistan. Trace Elements and Electrolytes (Accepted).

Khan, Z. I., M. Ashraf, I. Javed and S. Ermidou-Pollet. 2006c.Transfer of sodium from soil and forage to sheep and goats grazing in a semiarid region of Pakistan. Influence of the seasons. Trace Elements and Electrolytes (In press).

Khan, Z. I., A. Hussain, M. Ashraf, M. Y. Ashraf, E. E. Valeem, and M. S. Akhtar. 2004b. Seasonal variation in soil and forage mineral concentrations in a semiarid region of Pakistan. Pakistan Journal of Botany, 36: 635-640

Khan, Z. I., A. Hussain, M. Ashraf, M. Y. Ashraf, L. R. McDowell, B. Huchzermeyer. 2006a. Copper nutrition of goats grazing native and improved pasture with seasonal variation in a semiarid region of Pakistan. Small Ruminant Research, (in press).

Khan, Z. I., A. Hussain, M. Ashraf, M. Y. Ashraf L.R McDowell. 2005c. Macro mineral status of grazing sheep in Punjab, Pakistan. Small Ruminant Research, (in press).

Khan,Z.I., M. Ashraf and A. Hussain: Evaluation of manganese status of grazing sheep in a semi-arid region of Pakistan. 2007.Trace elements and electrolytes (Accepted)

Khan, Z. I., M. Ashraf, A. Hussain, and L.R.McDowell. 2005a. Seasonal variation of   trace elements in a semiarid veld pasture. Communications in soil science and plant analysis.37:1471-1484

Khan, Z. I., M. Ashraf, I. Javed and S. Ermidou-Pollet: Transfer of sodium from soil and forage to sheep and goats grazing in a semiarid region of Pakistan. Influence of the seasons. 2007.Trace elements and electrolytes (Accepted)

Khan, Z I.,, A. Hussain, M. Ashraf and S. Ermidou-Pollet: Transfer of iron from soil and forage to sheep grazing in a semiarid region of Pakistan. Influence of the seasons and the period of sampling.2007.Trace elements and electrolytes (Accepted)

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Paramo region of Colombia. II. Trace minerals. Small Rumin. Res. 5: 23-34.

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Mineral status of soils, forages, and cattle in Nicaragua. I. Micro-minerals. Rev. Fac. Agron., 14: 73-89.

Yuan, X. L. S. L. Li, X. S. Piao, C. H. Lai, J. J. Zang, Y. H. Ding, L. J. Han, In K. Han. 2006. The Nutritional Value of Brown Rice and Maize for Growing Pigs.Asian-Aust. J. Anim. Sci. 19 : 892.

Khan, Z. I. M. Ashraf and A. Hussain. 2007. Evaluation of Macro Mineral Contents of Forages: Influence of Pasture and Seasonal Variation . Aust. J. Anim. Sci. (Accepted).

 

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