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Runoff of 1,3-dichloropropene from field plots exposed to simulated and natural rainfall

机译:暴露于模拟和自然降雨的田地中1,3-二氯丙烯的径流

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Runoff potential of a subsurface soil-injected volatile compound, such as the soil fumigant 1,3-dichloropropene (1,3-D), that diffuses rapidly through the soil profile has not been studied for potential to contaminate surface water bodies through edge-of-field runoff. The objective of this study was to measure the runoff of 1,3-D, a soil fumigant and nematicide, under severe rainfall conditions at a field study site near Blacksburg, Virginia. 1,3-D was injected into the Groseclose clay loam (clayey, mixed mesic Typic Hapludults) at a 30 cm (12 inch) depth on three replicate 0.04 ha test plots. Special considerations for 1,3-D were required to make a uniform application to each plot and maintain worst-case conditions (rainfall timing and plot conditions). The measured application rate was 367-kg/ha (32.4 gallons/acre), which is greater than the typical maximum rate for Telone II~(~R) uses on crops grown in the Southeastern United States. The study was conducted on a hydrologic group C soil with a 5% slope. The 2-hour simulated rainfall water input was 9.4 cm (4.7 cm/h), which is about a 1-in-50-year storm for Blacksburg, Virginia. Concentrations of 1,3-D measured in soil and air prior to the simulated rainfall event suggested that 1,3-D was present at the soil surface and available for runoff. An average of 0.002% of the applied 1,3-D was observed in runoff. Maximum 1,3-D concentration (sum of both isomers) observed in runoff was 17.2 ppb, which is more than one order of magnitude below the lowest aqueous toxicological level of concern (280 ppb).
机译:尚未研究地下注入土壤的挥发性化合物(如土壤熏蒸剂1,3-二氯丙烯(1,3-D))在土壤剖面中快速扩散的径流潜力,该径流可能通过边缘土壤污染地表水体。野外径流。这项研究的目的是在弗吉尼亚州布莱克斯堡附近的野外研究场址下,测量1,3-D(土壤熏蒸剂和杀线虫剂)的径流。在3个重复的0.04公顷试验田中,以30厘米(12英寸)的深度将1,3-D注入Groseclose粘土壤土(粘土,混合的典型Typic Hapludults)中。需要对1,3-D进行特殊考虑,以便对每个样地进行统一应用并维持最坏情况(降雨时间和样地条件)。测得的施用量为367千克/公顷(32.4加仑/英亩),高于Telone II〜(R)在美国东南部种植的农作物上使用的典型最大施用量。该研究是在坡度为5%的C组水文土壤上进行的。 2小时的模拟降雨水输入为9.4厘米(4.7厘米/小时),大约是弗吉尼亚州布莱克斯堡的1年50年风暴。在模拟降雨事件发生之前在土壤和空气中测得的1,3-D浓度表明,土壤表面存在1,3-D,可用于径流。在径流中观察到平均为所施加的1,3-D的0.002%。在径流中观察到的最大1,3-D浓度(两种异构体的总和)为17.2 ppb,比所关注的最低含水毒理学水平(280 ppb)低一个数量级。

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