首页> 外文期刊>Journal of Science and Technology of Agriculture and Natural Resources >Nitrogen and Phosphorous Loss as Affected by Plough Direction in Rainfed Wheat Land of a Semi- Arid Region
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Nitrogen and Phosphorous Loss as Affected by Plough Direction in Rainfed Wheat Land of a Semi- Arid Region

机译:氮和磷损失受到半干旱地区雨水小麦土地的影响

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Sloping farmlands are the major sources of soil, water and nutrient losses in arid and semi-arid regions. Information about the impacts of different tillage practices on soil erosion, nutrient loss and crop nutrient uptake on the sloping farmland of semi- arid soil is, however, limited. This study was carried out to investigate the effects of tillage direction on soil, water, nitrogen and phosphorous losses and their uptake by plant in a rainfed wheat land. Field experiments were conducted in two tillage directions: downslope tillage and contour line tillage with four fertilization treatments: control, urea, triple superphosphate, and urea + triple superphosphate at the field plots with 1.75 m 8 m in dimensions by using the randomized completely block design at three replications in Zanjan Township during 2014-2015. According to the results, Significant differences were found between the two tillage practices in soil loss (P < 0.001), water loss (P < 0.001), nitrogen loss soil loss (P < 0.001), and nitrogen uptake by wheat grain (P < 0.001), while phosphorous loss and its uptake did not show any statistically significant difference. Soil and water loss in the downslope tilled plots was 1.65 and 2.50 times higher than the contour line tillage, respectively. Nitrogen loss in the downslope tilled plots was 1.29 times more than that in the contour line tilled plots. Nitrogen loss in the plots was attributed to soil and water loss, so significant relationships were observed between nitrogen loss and soil loss (R~(2) = 0.59) and water loss (R~(2) = 0.55). This study, therefore, revealed that the tillage direction is an important factor controlling runoff, soil loss, and nitrogen loss and its uptake by wheat in the rainfed lands of semi-arid regions. Application of the contour tillage is, therefore, the first step to conserve soil and water and to improve soil productivity in these regions.
机译:倾斜的农田是干旱和半干旱地区的土壤,水和养分损失的主要来源。然而,有关不同耕作实践对半干旱土壤倾斜农田土壤侵蚀,养分损失和作物营养吸收的信息,是有限的。进行了该研究,以研究耕种对土壤,水,氮气和磷损失的影响及其在雨水土地中的植物的吸收。现场实验以两种耕作方向进行:下升流耕作和轮廓线耕种,具有四种施肥处理:通过使用随机完全块设计,对照,尿素,三重磷酸盐和尿素在尺寸下的尺寸为1.75米8米处在2014 - 2015年Zanjan乡的三次复制。根据结果​​,在土壤损失两种耕作实践(P <0.001),水分损失(P <0.001),氮损失土壤损失(P <0.001)和小麦籽粒的氮气吸收之间发现了显着差异(P <0.001)(P < 0.001),而磷损失及其摄取没有显示出任何统计学上的差异。下坡耕地图中的土壤和水分损失分别比轮廓线耕作高1.65和2.50倍。下坡耕地图中的氮气损失比轮廓线耕种图中的1.29倍。地块中的氮气损失归因于土壤和水分损失,因此在氮气损失和土壤损失之间观察到显着的关系(R〜(2)= 0.59)和水分(R〜(2)= 0.55)。因此,这项研究表明,耕作方向是控制径流,土壤损失和氮气损失的重要因素,并在半干旱地区的雨水落地中用小麦的吸收。因此,在轮廓耕作的应用是节省土壤和水的第一步,并改善这些地区的土壤生产率。

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