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首页> 外文期刊>Journal of Agricultural Science >Simulating Soil Moisture under Different Tillage Practices, Cropping Systems and Organic Fertilizers Using CropSyst Model, in Matuu Division, Kenya
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Simulating Soil Moisture under Different Tillage Practices, Cropping Systems and Organic Fertilizers Using CropSyst Model, in Matuu Division, Kenya

机译:使用CropSyst模型在不同耕作方式,耕作制度和有机肥料下模拟土壤水分,肯尼亚马图乌省

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Soil moisture stress is a limiting factor in crop production particularly in arid and semi-arid lands (ASALs) as it affects many physiological and biochemical processes of plants. Research on moisture conservation measures is thus imperative. The current study used CropSyst model to simulate soil moisture under different tillage practices (oxen plough, tied ridges and furrows and ridges), cropping systems (monocropping, intercropping and crop-rotation) and organic fertilizers; farm yard manure, rock phosphate (RP) and Farmyard manure (FYM) combined with rock phosphate (RP+FYM). The study was conducted in Matuu Division, Kenya for two seasons; October 2012 to February 2013 short rain season (SRS) and March to August 2013 long rain season (LRS). The experiment was laid out in a Randomized Complete Block design with a split-split plot arrangement and replicated three times. The main plots were tillage practices whereas the split plots were cropping systems and split-split plots were organic fertilizers and a control (nothing applied). The test crops were sorghum ( Sorghum bicolor L.) and sweet potato ( Ipomea batatas L. lam ) rotated and/or intercropped with dolichos ( Lablab purpureus ) and chickpea ( Cicer arietinum ). The CropSyst model was calibrated using measured soil texture, permanent wilting point, bulk density and initial soil moisture at the experimental site. Model validation was done using Root Mean Square Error (RMSE), percentage differences (PD) and willmott index (WI) of agreement. CropSyst model was reasonably validated as indicated by the low RMSE (0.5 to 1.3), PD (less than ±15) and WI index (close to 1). In the first season and second season, simulated soil moisture (101.91 and 108.3 mm) was significantly (P < 0.05) high in sorghum/dolichos intercrop with RP+FYM application under tied ridges and least (13.52 and 15.4 mm) in control treatment of sorghum mono crop under oxen plough. In sweet potato plots, both individual treatment and treatment interaction significantly influenced simulated soil moisture. Sweet potato-dolichos rotation (75.32 and 79.63 mm), with application of RP+FYM (75.03 and 79.39 mm) under tield ridges (95 and 100.24 mm) had highest simulated soil moisture levels under oxen plough (32.49 and 34.36 mm), sweet potato monocrop (53.46 and 55.26 mm) and control (52.52 and 55.39 mm) having the least during the first and second season, respectively. In both sorghum and sweet potato based cropping systems, soil moisture was correspondingly highest in tied ridges, intercropping and rotation systems involving dolichos and application of FYM+RP and least in control of monocropping under oxen plough. Information on effects of tillage practices, cropping systems and organic inputs could be very useful for soil water conservation purposes. Thus, using simulation models to attain the same could be the ultimate solution. A good agreement between observed and simulated soil moisture implied that CropSyst model is capable of investigating sustainable alternatives of increasing soil moisture in the ASALs.
机译:土壤水分胁迫是作物生产的限制因素,特别是在干旱和半干旱地区(ASAL),因为它会影响植物的许多生理和生化过程。因此,必须研究保湿措施。当前的研究使用CropSyst模型来模拟不同耕作方式(牛犁,绑垄,犁沟和垄),耕作系统(单作,间作和轮作)和有机肥料下的土壤水分;农场肥料,磷矿石(RP)和农场肥料(FYM)与磷矿石(RP + FYM)结合使用。这项研究在肯尼亚的马图分部进行了两个季节。 2012年10月至2013年2月为短雨季(SRS)和2013年3月至2013年8月为长雨季(LRS)。该实验采用随机完整块设计进行设计,并采用分缝图布置,重复了3次。主要地块是耕作方式,而分开的地块是种植系统,分开的地块是有机肥料和对照物(未施肥)。试验作物为高粱(Sorghum bicolor L.)和甘薯(Ipomea batatas L. lam),轮作和/或间种有小菜蛾(Lablab purpureus)和鹰嘴豆(Cicer arietinum)。使用测量的土壤质地,永久性枯萎点,堆积密度和初始土壤湿度对CropSyst模型进行了校准。使用均方根误差(RMSE),百分比差异(PD)和Willmott指数(WI)进行模型验证。通过低RMSE(0.5至1.3),PD(小于±15)和WI指数(接近1)表明,CropSyst模型得到了合理验证。在第一季和第二季,高粱/白/间作模拟土壤水分(101.91和108.3 mm)在绑垄下施用RP + FYM显着高(P <0.05),而在对照处理中最低(13.52和15.4 mm)。高粱耕作下的高粱单作物。在甘薯地块中,单独的处理和处理之间的相互作用都极大地影响了模拟土壤的水分。在铁犁垄(95和100.24 mm)下施用RP + FYM(75.03和79.39 mm),甘薯-白垩纪轮作(75.32和79.63 mm)在牛犁(32.49和34.36 mm)下具有最高的模拟土壤湿度第一季和第二季的马铃薯单作(53.46和55.26毫米)和对照(52.52和55.39毫米)分别最少。在以高粱和甘薯为基础的耕作系统中,土壤水分在绑垄,间作和轮作系统中最高,其中包括连根土和施用FYM + RP,而在控制耕作的情况下最少。有关耕作实践,耕作制度和有机投入的影响的信息对于土壤水保护目的可能非常有用。因此,使用仿真模型获得相同的结果可能是最终的解决方案。观测到的土壤水分与模拟土壤水分之间的良好一致性意味着CropSyst模型能够研究ASAL中增加土壤水分的可持续替代方案。

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