I. INTRODUCTION
Halophytes are among the most salt-tolerant plants. These species can tolerate extreme conditions of aridity, salinity, and high temperatures [1]. In many areas of the world, halophytes are indispensable sources of animal feed, particularly in arid and semiarid climates. Such species can alleviate feed shortages, or even fill feed gaps during dearth periods, when annual grassland growth is limited or dormant due to unfavourable weather conditions [2, 3].
Livestock production practice in Algerian steppes is mainly based on grazing natural vegetation. The native rangelands of the country are greatly affected by annual precipitation, which is irregular and poorly distributed. The rangelands are characterized by a short rainy season, usually not more than three to four months per year [4]. Halophyte species are an important source for providing minerals to grazing livestock in extensive dearth situations. At the same time, mineral deficiencies can inhibit forage digestibility and herbage intake and ultimately decreases livestock production efficiency [5].
In Algeria, animal production is the main source of income for nomads. It relies mostly on natural vegetation for feeding sheep and goats [4]. In 2010, there were 18 million sheep in the Algerian steppe, which represents more than 86% of the total livestock population [6].
Feed sources of minerals are generally divided into various base feedstuffs, such as range or pasture plants, harvested forages, concentrates, and mineral supplements. However, efforts to minimize the cost of mineral supplementation in livestock production require a thorough knowledge of the supply and availability of mineral nutrients in feed and forages [7].
The instrumental neutron activation analysis (INAA) occupies a prominent position among various analytical methods due to its advantages of low detection limit, multi-elemental capability, a non-destructive method, and no sample preparation is required for analysis [8].
Traganum nudatum Del (Chenopodiaceae) is a native halophytic shrub in arid zones of the Mediterranean basin [9, 10]. To our knowledge, there are no published studies focusing on the chemical composition of T. nudatum, despite its forage value and importance in North African steppes. Therefore, the purpose of the present study was to assess chemical element contents in T. nudatum, mostly grazed by livestock in arid steppe of Algeria. This information may be used for the development of efficient chemical element supplementation regimes for grazing livestock.
II. MATERIALS AND METHODS
A. Study area
Foliage samples of T. nudatum were collected from the area of Mesrane in the province of Djelfa (3;03;E longitude, 34;36;N latitude and 830 m elevation) covered by a plant community, including Atriplex halimus, Suaeda fruticosa, and Salsola vermicular found in the Northern steppe of Algeria. The climate is typically Mediterranean, characterized by wet winters and hot dry summers with a mean annual precipitation of 250 mm/year. The average minimum winter and maximum summer temperatures are 5 ℃ in January and 26 ℃ in July, respectively. According to Halitim [11] the principal types of soil in the Mesrane zone are the calci-magnesic solontchak and isohumic soils.
B. Plant collection and sample preparation
Three 100 m transects were laid across the population of T. nudatum. These transects were further divided into three random blocks. Ten plants from each block were randomly harvested to measure chemical element content. Plant samples were clipped with stainless steel scissors with Teflon coated blades and, consequently, these samples were packed into paper bags. The samples were brought to the laboratory and were washed with distilled de-ionized water to remove any surface contamination and dried for 48 h in an oven at 60 ℃. The dried samples were ground to a fine powder in a high speed mill (IKA + A11 basic) to a particle size fraction of <200 μm. In order to minimize the contamination of Fe, Co, and Zn, dismountable Teflon coated blades were used for grinding.
Powdered plant samples were then stored in sterilized labeled polyethylene bottles and screw capped tightly to avoid absorption of moisture and any external contamination.
C. Instrumental Neutron Activation Analysis
The method used for the determination of chemical element mass fractions was a comparative (relative) neutron activation analysis, where both samples and standards were analyzed (irradiated and measured) under the same conditions. About 100 mg of the sample were sealed in quartz vials packed in aluminum containers and irradiated in the core of the reactor. For homogeneity, each sample was included in the mixture of 30 sample plants (i.e., 30 plants per transect). Three samples of plant material, together with triplicate CRM-GBW 07605 (GSV-4 tea leaves), were irradiated in the vertical channel of a multi-purpose, heavy-water research reactor (MHWRR) at a power of 5 MW, with a thermal neutron flux of 4.5×1013 cm-1 s-1 for 6 h, to carry out irradiation enough to activate the middle- and partially long-lived radionuclides in the samples. Before collecting data, a decay of 4 days and 4 weeks for the middle-lived and long-lived nuclides, respectively, was necessary. The powder was then put into new polypropylene capsules and reweighed. Both long and middle lived radionuclides were measured using a CANBERRA (HPGe p-type) coaxial detector and a CANBERRA inspector 2k. The system has a resolution (FWHM) of 1.87 keV for 1332.5 keV γ-peaks of 60Co and a relative efficiency of 35% when operated by Genie 2k software, with a low dead time (< 5%). The data transferred from the inspector to the computer were processed using the Genie 2000 software. Middle-lived radionuclides (Na, K, and Zn) were measured after 4 days; the collection time was 3600 s for each sample and each standard. Whereas, the long-lived radionuclides (Ca, Fe, Co, Eu, Sb, and Sc) were measured after 4 weeks for a collection time of 7200 s. Table 1 presents radionuclides, possible interferences, and gamma-energy used in this study.
Elements | Radionuclide | Half lifea | γ-peaks used (keV) | Possible interferences |
---|---|---|---|---|
Ca | 47Ca | 4.536 d | 1297.06 | No interferences |
K | 42K | 12.36 h | 1524.7 | No interferences |
Na | 24Na | 14.96 h | 1368.63 | 77Ge (1367.4) |
Zn | 69Zn | 13.76 h | 438.63 | 147Nd (439.40) |
Fe | 59Fe | 44.503 d | 1099.25 | 116In (1097.33) |
1291.6 | 116In (1293.56) | |||
Co | 60Co | 5.27 y | 1173.24 | No interferences |
1332.5 | No interferences | |||
Eu | 154Eu | 8.59 y | 123.07 | 171Er (124.02) |
1274.4 | 29Al (1273.37) | |||
Sb | 122Sb | 2.72 d | 564.12 | 134Cs (563.25) |
124Sb | 60.2 d | 602.73 | No interferences | |
Sc | 46Sc | 83.79 d | 889.28 | No interferences |
46Sc | 1120.54 | 182Ta (1121.3) | ||
48Sc | 43.67 h | 983.52 | No interferences | |
48Sc | 1312.1 | 160Tb (1312.14) |
III. RESULTS AND DISCUSSION
A. Chemical element contents
This investigation was conducted to determine the chemical element contents of T. nudatum used for animal gazing in the arid steppe of Algeria, in order to gain information on the deficiency and/or excess of mineral levels for ruminants grazing therein, fed mainly with this halophytic species.
Nine chemical elements were characterized in T. nudatum using INAA. Table 2 represents a comparison of our results for the reference materials to their certified values. For most of the elements, no significant discrepancy was observed between the measured concentrations and reference values. In order to evaluate the laboratory performance, we have determined the U-score test. This parameter is calculated according to the following equation
Elements | CRM-GBW 07605 (GSV-4 tea leaves) | |||
---|---|---|---|---|
Certified value | Measured value | Relative difference (%) | U-Score | |
[1pt] Ca | 4300 ±200 | 3850 ± 700 | 90 | 0.62 |
Co | 0.18 ± 0.02 | 0.18 ± 0.01 | 100 | 0.01 |
Eu | 0.018 ± 0.002 | 0.015 ± 0.003 | 83 | 0.83 |
Fe | 264 ± 10 | 254 ± 12 | 96 | 0.63 |
K | 16600 ± 600 | 16726 ± 1839 | 100 | 0.07 |
Na | 44 ± 4 | 61 ± 8 | 139 | 1.90 |
Sb | 0.06 ± 0.01 | 0.06 ± 0.01 | 100 | 0.01 |
Sc | 0.085± 0.009 | 0.096± 0.002 | 113 | 1.19 |
Zn | 26.3 ± 0.9 | 28.8 ± 1.03 | 109 | 1.85 |
where xlab and σlab are the laboratory measured value and the standard uncertainty of the laboratory measured value, respectively; xref and σref are the certified value and the standard uncertainty of the certified value, respectively.
A U-score ࣘ1 is satisfactory (the result is in agreement with the certified value); and unsatisfactory (the result and certified value are not in agreement) if the U-score >3.29 [12]. This evaluation shows the good quality of the results obtained in this investigation (Table 2).
The results are presented in Table 3 where all mass fractions are reported on dry mass basis as the averages of at least three independent determinations with standard errors of mean (SEM). The chemical element contents quantified in T. nudatum follow the trend in a descending order: Na > K > Ca > Fe > Zn > Co > Sb > Sc > Eu.
Elements | Mass fraction on dry mass basis |
---|---|
Ca (g/kg) | 1.00 ± 0.30 |
K (g/kg) | 1.10 ± 0.40 |
Na (g/kg) | 10.25 ± 1.95 |
Zn (mg/kg) | 15.30 ± 0.60 |
Fe (mg/kg) | 793 ± 38 |
Co (mg/kg) | 0.31 ± 0.04 |
Eu (mg/kg) | 0.033 ± 0.005 |
Sb (mg/kg) | 0.034 ± 0.007 |
Sc (mg/kg) | 0.170 ± 0.02 |
Na and K have an electrochemical function in ruminants and are associated with maintenance of acid–base equilibrium, membrane permeability and the osmotic control of water in the body [13]. Mass fractions of K were high and adequate for ruminants, exceeding the critical level of 0.65% of diet dry matter, as recommended by the National Research Council (NRC) [14]. These results were in agreement with those found previously by Del Valle and Rosell [15] in shrubs growing in Northeastern Patagonia.
T. nudatum had Na contents well above the needs of a growing adult range ruminant (0.1 g of Na kg-1 of diet dry matter for sheep). As stated by Masters et al. [16], small ruminants can tolerate a soluble salts intake in forage of about 100–150 g/day, provided that they have accessed to abundant water. High salt content is perhaps the major negative component in halophytic species. Therefore, mixing some halophytes with glycophyte forages is recommended for better utilization of saltbushes [5].
The Ca requirement for ruminants is 0.51% of diet dry matter, according to the NRC [14]. The results showed that the Ca mass fractions were higher than this requirement, therefore Ca deficiency would not be expected. Similar high forage Ca mass fractions were reported by Towhidi et al. [17] in other halophytes growing in a central arid zone of Iran.
T. nudatum contained Fe levels in substantial amounts to meet adult range ruminant requirements (45 mg of Fe kg-1 of diet dry matter for sheep). Similar findings were reported by Ogebe and McDowell [18] and Khan et al. [19], who evaluated the Fe contained in native forages that grow respectively in semiarid regions of Nigeria and Pakistan.
It has been suggested that forage crops containing more than 27 mg of Zn kg-1 of diet dry matter will protect livestock from Zn deficiency disorders [14]. In the present investigation, Zn mass fractions were sufficiently adequate for ruminant requirements. Other studies have found that browse halophytes from northern Brazil [20], arid regions of Jordan [21], and southern Tunisia [22] had sufficient amounts of Zn to meet requirements of adult range ruminants.
Co is often the most severe element deficiency of grazing livestock [13]. However in this study, T. nudatum had Co contents that were sufficient to meet adult range ruminant requirements (0.1 mg of Co kg-1 of diet dry matter for sheep). These results were in sharp contrast to those reported by Chelliah et al. [23] who found poor forage Co mass fractions (<0.1 mg/kg) in North Florida.
The Sc, Sb, and Eu elements in T. nudatum are present in the descending mass fractions as Sc > Sb > Eu (Table 3). This halophyte is quantified with the lowest Sc, Sb, and Eu contents, with respective values of per-mode=symbol, 0.17, 0.033 and 0.034 mg/kg, and were far below the tolerable weekly intake recommended by the NRC [14]. Therefore, its toxic effects will be negligible. Similar low Sc, Sb, and Eu mass fractions were reported recently by Nordløkken et al. [24] in native species growing in southwest Norway.
B. Potential of ruminant mineral intake
Table 4 shows the potential of chemical element intakes and daily chemical element requirements by ruminants from the leaves of T. nudatum. It seems that a sheep weighing about 50 kg and consuming 2.0 kg per day DM of this halophytic species could eat substantial amounts of Ca, K, Fe, Zn, and Co to meet their requirements.
Elements | Potential chemical element intakes per day a | Daily chemical element requirements b |
---|---|---|
Ca | (2 ± 0.62) g/kg | 0.51 g/kg |
K | (2.20 ± 0.82) g/kg | 0.65 g/kg |
Na | (20.25 ± 1.22) g/kg | 0.10 g/kg |
Zn | (30.6 ± 1.2) mg/kg | 27.00 mg/kg |
Fe | (1586 ± 76) mg/kg | 45.00 mg/kg |
Co | (0.62 ± 0.08) mg/kg | 0.10 mg/kg |
IV. CONCLUSION
Based on the present investigation, it is concluded that the T. nudatum saltbush contains adequate amount of chemical elements for livestock grazing in the arid steppes of Algeria. As a result, there is no urgent need for supplementation, as these elements are sufficient for ruminant requirements. However, offering fresh drinking water to animals fed T. nudatum saltbush would reduce Na intake and also enhance halophyte consumption and nutrients utilization.
Utilization of fodder trees and shrubs in the arid and semiarid zones of West Asia and North Africa
. Arid Soil Res Rehab, 2000, 14: 101-135. DOI: 10.1080/089030600263058Evolution of halophytes: multiple origins of salt tolerance in land plants
. Func Plant Biol, 2010, 37: 604-612. DOI: 10.1071/FP09269Effects of calcium chloride on growth, membrane permeability and root hydraulic conductivity in two Atriplex species grown at high (sodium chloride) salinity
. J Plant Nutr, 2009, 32: 1818-1830. DOI: 10.1080/01904160903242342Rangeland improvement and management options in the arid steppes of Algeria
. In:Halophytes and salt-tolerant plants as potential forage for ruminants in the Near East region
. Small Rum Res, 2010, 91: 3-12. DOI: 10.1016/j.smallrumres.2010.01.010Analytical methods for heavy metals in herbal medicines
. Phytoch Anal, 2011, 22: 189-198. DOI: 10.1002/pca.1287Biodiversity of halophytic vegetation in Chott Zehrez lake of Djelfa (Algeria)
. AmerJ Plant Sci, 2012, 3: 1527-1534. DOI: 10.4236/ajps.2012.311184Quality control and performance evaluation of k0-based neutron activation analysis at the Portuguese research reactor
. Nucl Instrum Meth Phys Res A, 2010, 622: 392-398. DOI: 10.1016/j.nima.2010.04.003Mineral composition of perennial vegetation of shrub patches in Northeastern Patagonia
. Arid Soil Res Rehab, 2000, 14: 15-25. DOI: 10.1080/089030600263148Biosaline agriculture for forage and livestock production
. Agri Ecosys Environ, 2007, 119: 234-248. DOI: 10.1016/j.agee.2006.08.003Nutritive value of some herbage for dromedary camels in the central arid zone of Iran
. Trop Animal Health Prod, 2011, 43: 617-622. DOI: 10.1007/s11250-010-9741-9Mineral concentrations of forages grazed by small ruminants in the wet season in benue state, Nigeria. II. Trace minerals and forage crude protein
. Comm Soil Sci Plant Anal, 1998, 29: 1211-1220. DOI: 10.1080/00103629809370021A study on seasonal variability of trace elemental status of forages for grazing ruminants
. J Plant Nutr, 2008, 31: 1345-1354. DOI: 10.1080/01904160802224425Neutron activation analysis of zinc in forages used in intensive dairy cattle production systems
. J Radioanal Nucl Chem, 2002, 252: 585-587. DOI: 10.1023/A:1015875309037Mineral assessment in Atriplex halimus L. and Atriplex nummularia L. in the arid region of Jordan
. Afr J Range Forage Sci, 2003, 20: 247-251. DOI: 10.2989/10220110309485822A survey of chemical and nutritional characteristics of halophytes plants used by camels in Southern Tunisia
. Trop Animal Health Prod, 2009, 41: 209-215. DOI: 10.1007/s11250-008-9177-7Mineral concentrations of cool season pasture forages in North Florida during the winter-spring grazing season: II. trace minerals
. J Plant Nutr, 2008, 31: 1774-1788. DOI: 10.1080/01904160802324902Essential and non-essential elements in natural vegetation in southern Norway: Contribution from different sources
. Sci Total Environ, 2015, 502: 391-399. DOI: 10.1016/j.scitotenv.2014.09.038