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首页> 外文期刊>Brazilian Journal of Soil Science >Erosivity, hydrological patterns, return period and probability of occurrence of rainfalls at Sao Borja, RS, Brazil.
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Erosivity, hydrological patterns, return period and probability of occurrence of rainfalls at Sao Borja, RS, Brazil.

机译:巴西圣保罗州的侵蚀力,水文模式,返回期和降雨发生的可能性。

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摘要

The erosivity potential of rainfalls can be estimated by some indexes, among them the EI30, which is given by the product of kinetic energy (E) and rainfall intensity for a 30-minute period (I30). The purpose of this study was to determine rainfall erosivity, hydrological patterns, return period and probability of occurrence of erosive rainfalls in Sao Borja, Rio Grande do Sul, Brazil, based on diary rainfall charts of the FEPAGRO meteorological station, from 1956 to 2003. The duration and accumulated amount of each erosive rainfall were measured, entered in a spreadsheet, digitalized and processed by CHUVEROS software, which calculated the EI30 index and the monthly and annual total erosivity, besides determining the hydrological pattern of each rainfall. Most of the annual erosivity (76%) was concentrated between October and April, in the period of soil tillage, sowing and growth of summer crops. The most notable peak in the erosive potential was observed between March and April (1260-1269 MJ mm/ha/h), when most crops are normally in full growth, while July and August were the months of lowest erosive potential (268-271 MJ mm/ha/h). Of the total erosive rainfalls 47, 25 and 28% had advanced, intermediary and delayed patterns, respectively, while these patterns corresponded to 50, 26 and 24%, respectively, of the mean annual volume of erosive rainfalls and to 53, 25 and 22% of the average annual erosivity. The mean annual index of erosivity in Sao Borja is 9751 MJ mm/ha/h/year. It represents the 'R' Factor of the Universal Soil Loss Equation to be used in Sao Borja and regions with similar rainfall pattern. Linear and potential regressions were obtained to express the mean annual EI30 index by pluviometric records expressed as rainfall coefficient. The mean annual rainfall erosivity index of 9751 MJ mm/ha/h/year (Factor 'R' of USLE for Sao Borja, RS, Brazil), is expected to occur once every 2.2 years, with a 44.9% likelihood.
机译:降雨的侵蚀力潜力可以通过一些指标来估算,其中包括EI30,它是由动能(E)和30分钟内降雨强度(I30)的乘积给出的。这项研究的目的是根据FEPAGRO气象站1956年至2003年的日记降雨图,确定巴西南里奥格兰德州圣博尔哈市的降雨侵蚀力,水文模式,恢复期和发生侵蚀性降雨的可能性。测量每次侵蚀性降雨的持续时间和累积量,将其输入电子表格,然后通过CHUVEROS软件进行数字化处理,计算出EI30指数以及月度和年度总侵蚀性,并确定每种降雨的水文模式。在土壤耕作,播种和夏季作物生长期间,大部分年度侵蚀力(76%)集中在10月至4月之间。在3月和4月之间(1260-1269 MJ mm / ha / h)观察到了最大的侵蚀潜力峰值,当时大多数农作物通常都处于完全生长状态,而7月和8月则是侵蚀潜力最低的月份(268-271) MJ mm / ha / h)。在总侵蚀性降雨中,有47%,25%和28%分别具有高级,中间和延迟模式,而这些模式分别相当于年平均侵​​蚀性降雨量的50%,26%和24%,分别相当于53、25和22%。年平均腐蚀率的百分比。圣博尔哈州的侵蚀力年平均指数为9751 MJ毫米/公顷/小时/年。它表示将在圣博尔哈和降雨模式相似的地区使用的通用土壤流失方程的“ R”因子。通过雨量记录将降雨指数表示为线性和潜在回归值,以表示年平均EI30指数。每年平均降雨侵蚀力指数为9751 MJ mm / ha / h /年(巴西圣保罗的USLE的“ R”因子),预计每2.2年发生一次,可能性为44.9%。

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