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首页> 外文期刊>Agricultural Journal >Agro-Ecological Study of the Plain of M?sila, Western Northern Zone of the Basin of Hodna, Wilaya of M?sila, Algeria
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Agro-Ecological Study of the Plain of M?sila, Western Northern Zone of the Basin of Hodna, Wilaya of M?sila, Algeria

机译:阿尔及利亚霍西纳盆地西部北部地带,西拉平原,西拉平原的农业生态研究

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摘要

Algeria is vast country which presents several bioclimatic stages and agro-ecological which supports the production, a multitude of agricultural produce. The steppe forms integral part of this extent of which importance is hardly lower than the other areas. Hodna is in the middle of the Algerian steppe, it is a relatively degraded basin of 25000 km2, consequence of a prolonged dryness and an overgrazing. This study is devoted to the diagnosis of the current location of the perimeter of the plain of M?sila which is in the Western Northern zone of the basin of Hodna on a geographical area of a surface of 780 km2. The population is dense in North with the existence of an urban centre and a relatively populated rural area in the South, the population is less dense with relatively distant urban centers. The plain of M?sila receives an annual rain average of 213.20 mm, the rains of Autumn are sometimes torrential which gives birth to abrupt risings and devastators. The thermal amplitude of the station of M?sila is of 35.02°C. The dominant winds are the wind of West known as Dahraoui, wind of North known as Bahri and the Sirocco which is hot wind and blowing dryness of the South and which blocks the development of the cultures by accentuating their drying. The diagram ombrothermic allows to identify existence; only one period of 3 months dryness, the end of May at the end of August. The zone study is made up an alluvial plain of low altitudes, <400 m made of alluvial deposits of quaternary (alluvia, clays and sands) with a soft slope <3%, pertaining to steppe bioclimatic stage. The ground is not very advanced of alluvial contribution with limono-argillaceous texture rather deep. Occupation of the ground by the vegetation is diversified, one noted a broad diversity of the agricultural activity which settled current the last years which exceeds 54,700 ha, the fallow exceed half of agricultural surfaces during the agricultural partner 2009/2010, the cultivation of cereals which occupies 36% of the grounds followed by the fodder cultures and fruit-bearing arboriculture at a rate of 5 and 4%, respectively. The exploration of the not cultivated plant species of the area study, counts 550 tax relating to the steppe communities with Chott El Hodna. One finds there many species endemic with the area of Hodna such as Saccocalyx saturoides, Arnebia decumbens and Linaria laxiflora that one finds only in this area. As well as endemic species North African such as Muricaria prostrata, Loncophora capiomontiana, Rhanterium suaveolens, Stippa tenacissima L., Artimisia herba alba, Anabasis oropediorum L., Salsola vermiculata L., Atriplex halimus and Salicornia arabica L. The zone of study, like the majority of the steppe zones is with vocation agropastorale with manpower of the ovine breeding bordering the 130.000. The zone study belongs to the large catchment area of Chott El Hodna, characterized by a very dense hydrographic network where the rivers take their sources in the mounts of Hodna, the principal river is El-K?sob. The near total of water of the plain of M?sila has a temperature which varies between 21.5 and 22°C, this translated by a strong corrosion of the casing of the drillings. The majority of water of this plain have a strong conductivity, therefore a degree of raised mineralization in the event of irrigation with this salt water charged one can expect falls of outputs.
机译:阿尔及利亚是一个幅员辽阔的国家,具有几个生物气候阶段和农业生态学,可支持多种农产品的生产。草原是这一程度不可或缺的一部分,其重要性几乎不比其他地区低。霍德纳(Hodna)位于阿尔及利亚大草原的中部,是一个相对退化的盆地,面积达25000 km2,这是干燥时间延长和过度放牧的结果。这项研究致力于诊断M?sila平原周界的当前位置,该平原位于Hodna盆地的西部北部地区,地理面积为780 km2。北部人口稠密,有城市中心,而南部人口相对较少,而人口密度较小,城市中心较远。 M?sila平原的年平均降雨量为213.20毫米,秋季的降雨有时是洪流,这会导致突然的上升和破坏。 M?sila站的热振幅为35.02°C。主导风是西方的Dahraoui风,北方的Bahri风和Sirocco风,它们是南方的热风和吹干性,并通过加剧干燥来阻碍文化的发展。这张图可以识别存在。干燥期只有3个月,5月底为8月底。该区域研究是由一个低海拔冲积平原组成的,该冲积平原<400 m由第四纪冲积沉积物(高岭土,粘土和沙子)构成,软坡度小于3%,属于草原生物气候阶段。地面的冲积作用不是很先进,其脂多糖质地较深。植被对地面的占用是多种多样的,有人指出,农业活动的多样性非常广泛,最近几年的耕地面积超过54,700公顷,农业合作伙伴2009/2010年的休耕面积超过农业面积的一半,谷物种植占36%的土地,其次是饲料培养和含水果的树木栽培,比例分别为5%和4%。探索该区域研究中未种植的植物物种,需要缴纳550笔与Chott El Hodna草原社区有关的税。人们发现在霍德纳地区有许多特有物种,例如沙棘(Saccocalyx saturoides),紫草(Arnebia decumbens)和拉纳里亚(Linaria laxiflora),只能在这一地区发现。以及北非的特有物种,例如Muricaria prostrata,Loncophora capiomontiana,Rhanterium suaveolens,Stippa tenacissima L.,Artimisia herba alba,Anabsis oropediorum L.,Salsola vermiculata L.,Atriplex halimus和Salicornia arabica L.等。大部分草原地区都设有农业农牧业,人工繁殖的绵羊有130.000头。区域研究属于霍特纳河大流域,其特征是水文网络非常密集,河流取自霍德纳山,主要河流是El-K?sob。 M?sila平原近乎全部的水温在21.5至22°C之间变化,这是由于钻井套管受到强烈腐蚀而引起的。该平原的大部分水具有很强的电导率,因此,如果使用这种盐水进行灌溉,则一定程度的矿化程度会提高,这可能会导致产量下降。

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