IMPACT OF TILE DRAINAGE SYSTEM AND WATER QUALITY ON SOME SOIL PROPERTIES AND CROP YIELDS OF WHEAT AND MAIZE

Mona K.M. Abdul-Razek, M. Abd-Eladl, H. Khafagy
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The laterals were constructed at 1.2 m depth and 30 m drain spacing with a length varies from 250-275 m. Five feddans in each area were selected to carry out this study. Moreover, nontiled drained areas were selected in both two areas as control areas. The results of irrigation water analysis revealed that generally, both fresh and mixed water applied in this study could be used safely according to the standard guidelines of FAO (1994) which means that, using such mixed water safely can save about 50% of fresh water needed for crop water requirements. Also the results proved that, at Mahallet Rooh area where fresh irrigation water is used, the soil salinity reduced by about 30.7% as compared with the initial value in the area not provided with tile drainage, but the reduction in soil salinity was about 58.9% in the area provided with tile drainage system. The total amounts of leached salts from the top 60 cm of soil were 1850.4 and 2051.8 kg/fed for nontiled and tiled areas of Mahllet Rooh area, respectively. Concerning Saft Torab area, where mixed water is used for irrigation, these amounts were 1222.1 and 1965.2 kg/fed for the top 60 cm of soil, respectively. The obtained results confirmed that, the tiled areas at Mahallet Rooh, where fresh irrigation water is applied, showed a relatively higher values of quickly drainable pores (QDP), slowly drainable pores (SDP) and consequently, the total drainable pores (TDP) as compared with that of Saft Torab area where mixed water is used for irrigation. On contrary, the water holding pores (I.e. fine and coarse capillary pores values) were relatively higher as compared with that of Mahallet Rooh area. The non-tiled areas in both Mahallet Rooh and Saft Torab showed almost the same values of pore size distribution components, but the fine capillary pores value (FCP) was slightly higher for Saft Torab as compared with that obtained for Mahallet Rooh area. The results showed that soil bulk density values were lower in areas provided with tile drainage either in Mahallet Rooh or Saft Torab area resulting higher total porosity values as compared with that not provided with tile drainage. The results indicate that water table levels during winter season were much deeper than that observed in summer season in both areas under this study. The tile drainage areas showed a pronounced effect on lowering water table level as compared with the areas that not provided with tile drainage system. The results indicate that using mixed irrigation water which has a relatively higher salt content caused a higher salinity of water table as compared with that of Mahallet Rooh area where fresh irrigation water is used. Mona K.M. Abdul-Razek, et al., 284 Drain spacing is calculated according to Hooghoudt equation using the field data measurements of soil hydraulic conductivity and water table levels midway between drains. The results revealed that, using the field data the calculated drain spacing was 27 m at Mahallet Rooh area, while it was to 30 m spacing at Saft Torab. The designed values were 30 m which is almost the same as the calculated values. These results indicate to the good performance of tile drains in both areas under the study according to the field actual measurements. 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引用次数: 0

Abstract

The current study was carried out in two successive seasons (winter 2015/2016 and summer 2016) on two areas (Mahallet Rooh and Saft Torab). Both areas belong to El-Santa District (about 13 km to Tanta, Gharbia Governorate, Egypt). This work was conducted in clay loam soils to study the feasibility of installing tile drainage at farm level and using fresh and mixed water (fresh and drainage water i.e.1:1) on some soil properties, wheat and maize productivity. Moreover, the obtained field data were used to evaluate the field drains through comparing the calculated drain spacing using Hooghoud equation with the actual drain spacing. Both areas have a covered drainage system. The laterals were constructed at 1.2 m depth and 30 m drain spacing with a length varies from 250-275 m. Five feddans in each area were selected to carry out this study. Moreover, nontiled drained areas were selected in both two areas as control areas. The results of irrigation water analysis revealed that generally, both fresh and mixed water applied in this study could be used safely according to the standard guidelines of FAO (1994) which means that, using such mixed water safely can save about 50% of fresh water needed for crop water requirements. Also the results proved that, at Mahallet Rooh area where fresh irrigation water is used, the soil salinity reduced by about 30.7% as compared with the initial value in the area not provided with tile drainage, but the reduction in soil salinity was about 58.9% in the area provided with tile drainage system. The total amounts of leached salts from the top 60 cm of soil were 1850.4 and 2051.8 kg/fed for nontiled and tiled areas of Mahllet Rooh area, respectively. Concerning Saft Torab area, where mixed water is used for irrigation, these amounts were 1222.1 and 1965.2 kg/fed for the top 60 cm of soil, respectively. The obtained results confirmed that, the tiled areas at Mahallet Rooh, where fresh irrigation water is applied, showed a relatively higher values of quickly drainable pores (QDP), slowly drainable pores (SDP) and consequently, the total drainable pores (TDP) as compared with that of Saft Torab area where mixed water is used for irrigation. On contrary, the water holding pores (I.e. fine and coarse capillary pores values) were relatively higher as compared with that of Mahallet Rooh area. The non-tiled areas in both Mahallet Rooh and Saft Torab showed almost the same values of pore size distribution components, but the fine capillary pores value (FCP) was slightly higher for Saft Torab as compared with that obtained for Mahallet Rooh area. The results showed that soil bulk density values were lower in areas provided with tile drainage either in Mahallet Rooh or Saft Torab area resulting higher total porosity values as compared with that not provided with tile drainage. The results indicate that water table levels during winter season were much deeper than that observed in summer season in both areas under this study. The tile drainage areas showed a pronounced effect on lowering water table level as compared with the areas that not provided with tile drainage system. The results indicate that using mixed irrigation water which has a relatively higher salt content caused a higher salinity of water table as compared with that of Mahallet Rooh area where fresh irrigation water is used. Mona K.M. Abdul-Razek, et al., 284 Drain spacing is calculated according to Hooghoudt equation using the field data measurements of soil hydraulic conductivity and water table levels midway between drains. The results revealed that, using the field data the calculated drain spacing was 27 m at Mahallet Rooh area, while it was to 30 m spacing at Saft Torab. The designed values were 30 m which is almost the same as the calculated values. These results indicate to the good performance of tile drains in both areas under the study according to the field actual measurements. The results revealed that, both grain and biological wheat and maize yields in drained areas and that irrigated with fresh water are higher than that obtained in non-drained areas and that irrigated with mixed water.
排水系统和水质对小麦和玉米部分土壤性质及作物产量的影响
目前的研究是在两个地区(Mahallet Rooh和Saft Torab)连续两个季节(2015/2016冬季和2016夏季)进行的。这两个地区都属于El-Santa区(距埃及加尔比亚省坦塔约13公里)。本研究在粘壤土中进行,以研究在农田水平安装瓦片排水和使用淡水和混合水(淡水和排水即1:1)对某些土壤性质,小麦和玉米生产力的可行性。通过Hooghoud方程计算的漏距与实际漏距的比较,利用获得的现场数据对现场漏距进行了评价。这两个地区都有覆盖的排水系统。分支井深度为1.2 m,排水间距为30 m,长度为250-275 m。在每个地区选择5个feddan进行本研究。此外,两个地区均选择了未平铺的排水区作为对照区。灌溉水分析结果表明,根据FAO(1994)的标准准则,本研究中使用的淡水和混合水一般都可以安全使用,这意味着安全使用这种混合水可以节省作物需水量所需淡水的50%左右。结果还表明,在Mahallet Rooh地区,使用新鲜灌溉水时,土壤盐分较未设置瓦片排水的初始值降低了约30.7%,而设置瓦片排水的地区土壤盐分降低了约58.9%。马勒路地区未铺地和铺地60 cm土壤淋溶盐总量分别为1850.4 kg/次和2051.8 kg/次。在采用混合水灌溉的Saft Torab地区,土壤顶部60 cm的土壤土壤含盐量分别为1222.1 kg/次和1965.2 kg/次。结果表明,与使用混合水灌溉的Saft Torab地区相比,Mahallet Rooh地区的平铺区快速排水孔(QDP)、缓慢排水孔(SDP)以及总排水孔(TDP)值相对较高。与Mahallet Rooh区相比,持水孔(即细孔和粗孔)相对较高。Mahallet Rooh和Saft Torab的非平铺区域的孔隙大小分布成分值几乎相同,但Saft Torab的细毛管孔隙值(FCP)略高于Mahallet Rooh区域。结果表明,在Mahallet Rooh和Saft Torab地区,采用瓦排水的土壤容重值较低,总孔隙度值高于未采用瓦排水的土壤。结果表明,两区冬季地下水位均明显高于夏季地下水位。与未设置瓦排水系统的地区相比,瓦排水区对降低地下水位的效果显著。结果表明,使用含盐量相对较高的混合灌溉水导致地下水位盐度高于使用新鲜灌溉水的Mahallet Rooh地区。Mona K.M. Abdul-Razek等,284排水间距是根据Hooghoudt方程计算的,使用的是土壤水力导电性和排水管道之间的地下水位的实地数据测量。结果表明,利用现场数据,Mahallet Rooh地区计算出的泄油间距为27 m,而Saft Torab地区计算出的泄油间距为30 m。设计值为30 m,与计算值基本一致。现场实测结果表明,研究区和试验区瓷砖排水管均具有良好的性能。结果表明,干旱区和淡水灌溉的粮食和生物小麦、玉米产量均高于非干旱区和混水灌溉的产量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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