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首页> 外文期刊>Global Journal of Agricultural Sciences >Preliminary studies of soil erosion in a valley bottom in Ibadan under some tillage practices.
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Preliminary studies of soil erosion in a valley bottom in Ibadan under some tillage practices.

机译:在一些耕作方式下伊巴丹山谷底部土壤侵蚀的初步研究。

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The effects of soil type and tillage interaction on nutrient loss in surface runoff and eroded soil, soil physico-chemical properties and maize growth and yield was assessed at a valley bottom in the University of Ibadan, Ibadan extends from Latitude 7 degrees 241 N to Longitude 3 degrees 54 E. Field experiments were carried out for four months on 5% slope as a 2x3 factorial in a randomized complete block design involving two soil types (Apomu and Osun series) as factors, each at three levels of tillage practices; stubble mulch tillage (ST), Traditional tillage (TT), and Zero tillage (ZT). Each tillage method occupied 22x5 m size erosion plot, which was replicated three times on each soil type. Pre-and post study soil samples were analysed for physical and chemical properties. The plots were sown to maize at 90 cm between and 30 cm within rows spacing under which runoff and soil loss from each plot were determined using soil and water collecting devices at the end of each plot. Results showed that soil bulk density at 0-30 cm soil depths was lower in ZT than ST and TT by 0.06 and 0.17 g/cm3 and 0.09 and 0.14 g/cm3 on Apomu and Osun series, respectively, after cropping cycle. Zero tillage was higher in moisture content than ST and TT on both Apomu and Osun series by (10.83; 11.67)% and (4.05; 8.77)%, respectively. The interaction between soil type and tillage had no significant effect on soil physical properties while it had effect on some soil nutrients: org. C, Ca, Mg, K and Zn. Although soil nutrients declined in all plots after cropping cycle but lowest declines were in ZT plot on both Apomu and Osun Series: Soil loss was higher in ST and TT than ZT by (56.27, 79.46)%, (30.36, 56.52)% on Apomu and Osun series, respectively. Corresponding runoff were (36.50; 52.38)% and (22.58; 26.52)% respectively for the Apomu and Osun series. Maize height, stem girth and leaf area index were in the following order: TT>ST>ZT on Apomu and Osun series with significant interaction (P<0.05). Maize grain yield was higher on TT than ST and ZT by (14.98; 11.56)% and (5.62; 15.08)% on Apomu and Osun series, respectively. Eroded soils and runoff water obtained from ST and TT plots were consistently richer in nutrient contents than ZT plots on both soil types. ZT could be a better option for soil and water conservation on Apomu and Osun series, which dominate the valley bottoms in Ibadan.
机译:在伊巴丹大学的一个谷底评估了土壤类型和耕作相互作用对地表径流和侵蚀土壤养分流失,土壤理化性质以及玉米生长和产量的影响。伊巴丹大学从纬度7度开始扩展了24度。 1 至经度3度54E。以2x3阶乘为因子,在5%坡度上进行了四个月的野外试验,涉及两个土壤类型(Apomu和Osun系列)作为随机因素的完全块设计。耕作实践的三个层次;秸秆覆盖耕作(ST),传统耕作(TT)和零耕作(ZT)。每种耕作方法占用22x5 m大小的侵蚀区,在每种土壤类型上重复3次。研究前后对土壤样品进行了理化性质分析。在行间距为90厘米至30厘米之间的地块播种玉米,在此间隔下,使用每个地块末端的土壤和水收集装置确定每个地块的径流和土壤流失。结果表明,ZT处0-30 cm土深处的土壤容重比ST和TT低0.06和0.17 g / cm 3 以及0.09和0.14 g / cm 3 分别在种植周期后对Apomu和Osun系列进行。在Apomu和Osun系列上,零耕作的水分含量分别比ST和TT高(10.83; 11.67)%和(4.05; 8.77)%。土壤类型和耕作之间的相互作用对土壤物理性质没有显着影响,而对某些土壤养分则有影响。 C,Ca,Mg,K和Zn。虽然在种植周期后所有地块土壤养分均下降,但在Apomu和Osun系列上ZT地块的下降幅度最小:ST和TT的土壤流失量比ZT高(Apomu的(56.27,79.46)%,(30.36,56.52)%和Osun系列。 Apomu和Osun系列的相应径流分别为(36.50; 52.38)%和(22.58; 26.52)%。玉米高度,茎周长和叶面积指数按以下顺序排列:Apomu和Osun系列上的TT> ST> ZT具有显着的相互作用(P <0.05)。 TT上的玉米籽粒产量比ST和ZT分别高(14.98; 11.56)%和Apomu和Osun系列的(5.62; 15.08)%。从ST和TT样地获得的侵蚀土壤和径流水在两种土壤类型上始终比ZT样地富含营养成分。在Ipodan谷底占主导地位的Apomu和Osun系列上,ZT可能是水土保持的更好选择。

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