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Role of Soil Clays for Watershed Management in Mewat Region of Haryana

机译:土壤粘土对流域管理的作用在哈里亚纳邦的Mewat地区

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Watershed management is an important technique for sustainable development of an area. A study was undertaken to assess the importance of clay fraction of soils in the management of Buraka micro-watershed in Mewat region of Haryana. The watershed is located in the foot hills of Aravallis comprising Buraka, Panchgaon and parts of Chila and Gwarka villages covering an area of 542.4 ha in Agro-ecological Subregion (AESR) No. 4.1. The elevation ranges from 259 to 340 m above MSL and slope varies from nearly level to steep, directed from south-east to north-west. The geology is sandstone and quartzite in hills and alluvium in plains. The area has been surveyed on 1:12,500 scale by using the Survey of India toposheets on 1:25,000 scale, cadastral maps on 1:4,000 scale and geo-coded IRS P6 LISSIVMSS imageries on 1:12,500 scale. Soil samples have been collected from different horizons of representative pedons as well as random (auger bores) observations in each interpreted physiographic units as per the heterogeneity of the terrains. Soil samples have been analysed for different physical and chemical properties using standard procedures. On the basis of image data interpretations and field checks seven landform units viz., hill tops, side slopes, inter hill basin, upper piedmont plain, middle (Buraka A to Buraka J) piedmont plain, lower piedmont plain and stream terraces have been identified in the study area. Ten soils have been identified and mapped into 21 soil mapping units as phases of soil series under Entisols and Inceptisols. The soil texture comprises sand, loamy sand, gravelly sandy loam and sandy loam covering 55.40 ha (10.22%), 133.90 ha (24.69%), 116.50 ha (21.48%) and 206.70 ha (38.10%), respectively. The soils ofAravalli hills are having gravelly sandy loam texture whereas in the plains it is sandy loam, loamy sand and sand. The particle size distribution i.e. sand, silt and clay ranges from 54.80 to 93.85%, 2.90 to 31.70% and 2.25 to 17.50%, respectively. The data also reveals that Buraka F soils (soil units 13 and 14) are having comparatively higher clay content (12.50 to 17.50% with a mean value of 16.38%), located in Buraka, Panchgaon and Chilla villages of the watershed area. Besides, these areas occur on nearly level to very gently sloping lands on relatively lower elevations. Hence, these areas of the watershed are potential for conserving water flown from uplands to down streams and can be used as water reservoirs for cultivation and livestock needs as well as for domestic use. On the basis of the present study, three sites have been identified for delineation of water harvesting zones for storing excess runoff water. This will help the farming community to meet their water requirements during the dry spells. By this way the chances of crops failure during droughts can be minimized and the agricultural productivity can be enhanced and sustained.
机译:流域管理是一个区域可持续发展的重要技术。开展了一项研究,以评估哈里亚纳岛Mewat地区Mulaka Micrat-satershed中土壤粘土分数的重要性。分水岭位于阿拉巴斯的脚山,包括布鲁卡,奇拉邦和吉拉和Gwarka村庄的一部分,占地面积542.4公顷的区域(AESR)4.1号。 MSL和坡度从259到340米的高程范围从近水平变化,从东南到西北部。地质是山丘和石英石的平原。该地区于1:12,500级调查,使用印度Toposheets的1:25,000规模,1:4,000规模和地理编码的美国国税局P6 Lissivmss Imageries,1:12,500规模上的Caadastral Maps。根据地球的异质性,已经从代表佩斯的不同视野以及各种解释的地理学单元的随机(螺旋钻孔)观察中收集了土壤样品。使用标准程序分析了土壤样品的不同物理和化学性质。在图像数据解释和现场检查七个地貌单位Ziz。,山顶,侧倾坡,山脉盆地,上部皮埃蒙特平原,中间(Buraka A到Buraka J)Piedmont Plain,下皮普通普通和流梯田已经确定了在研究区。由于奥斯索尔斯和最初的土壤系列阶段,已经确定了十个土壤和映射到21个土壤映射单元。土壤纹理包括沙子,壤土,砾石砂土和砂土覆盖物55.40公顷(10.22%),133.90公顷(24.69%),116.50公顷(21.48%)和206.70%(38.10%)。 Oravalli Hills的土壤具有砾石砂质壤土纹理,而在平原中,它是桑迪壤土,粘稠的沙子和沙子。粒度分布即,砂,淤泥和粘土分别为54.80%至93.85%,2.90至31.70%,分别为2.25至17.50%。该数据还揭示了南町土壤(土壤单元13和14)的粘土含量相对较高(12.50至17.50%,平均值为16.38%),位于海滨地区的布里卡,攀岩和奇拉村。此外,这些地区发生在几乎水平上,以非常轻微地倾斜的升降落地。因此,流域的这些领域是保护从高地向下流动的水的潜力,并且可以用作栽培和牲畜需求以及家庭使用的水库。在本研究的基础上,已经确定了三个地点用于描绘用于储存过量径流水的水收集区。这将有助于农业社区在干燥的法术中满足他们的水需求。通过这种方式,可以最小化干旱过程中的作物失效的机会,并且可以提高和持续农业生产力。

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