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Effect of variable annual precipitation and nutrient input on nitrogen and phosphorus transport from two Midwestern agricultural watersheds

机译:年降水量和养分输入量的变化对中西部两个农业流域氮磷运移的影响

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Precipitation patterns and nutrient inputs affect transport of nitrate (NO_3-N) and phosphorus (TP) from Midwest watersheds. Nutrient concentrations and yields from two subsurface-drained watersheds, the Little Cobb River (LCR) in southern Minnesota and the South Fork Iowa River (SFIR) in northern Iowa, were evaluated during 1996-2007 to document relative differences in timings and amounts of nutrients transported. Both watersheds are located in the prairie pothole region, but the SFIR exhibits a longer growing season and more livestock production. The SFIR yielded significantly more NO_3-N than the LCR watershed (31.2 versus 21.3 kg NO_3-Nha~(-1)y~(-1)).The SFIR watershed also yielded more TP than the LCR watershed (1.13 versus 0.51 kg TP ha~(-1) yr~(-1)), despite greater TP concentrations in the LCR. About 65% of NO_3-N and 50% of TP loads were transported during April-June, and <20% of the annual loads were transported later in the growing season from July-September. Monthly NO_3-N and TP loads peaked in April from the LCR but peaked in June from the SFIR; this difference was attributed to greater snowmelt runoff in the LCR. The annual NO_3-N yield increased with increasing annual runoff at a similar rate in both watersheds, but the LCR watershed yielded less annual NO_3-N than the SFIR for a similar annual runoff. These two watersheds are within 150 km of one another and have similar dominant agricultural systems, but differences in climate and cropping inputs affected amounts and timing of nutrient transport.
机译:降水方式和养分输入影响中西部流域硝酸盐(NO_3-N)和磷(TP)的迁移。 1996-2007年期间对两个地下排水流域(明尼苏达州南部的小柯布河(LCR)和爱荷华州北部的南福克爱荷华河(SFIR))的养分浓度和产量进行了评估,以记录养分时间​​和养分含量的相对差异运输。这两个流域都位于草原坑洼地区,但是SFIR的生长季节更长,牲畜产量更高。 SFIR分水岭产生的NO_3-N比LCR分水岭要多得多(31.2比21.3 kg NO_3-Nha〜(-1)y〜(-1))。SFIR分水岭也比LCR分水岭产生更多的TP(1.13对0.51 kg TP尽管LCR中的TP浓度较高,但ha〜(-1)yr〜(-1))。在4月至6月间运输了约65%的NO_3-N和50%的TP负荷,而在生长季节之后的7月至9月,运输了<20%的年负荷。 NO_3-N和TP的每月负荷在4月从LCR达到峰值,但在6月从SFIR达到峰值。这种差异归因于LCR中更大的融雪径流。在两个流域,年NO_3-N的产量都随着年径流量的增加而增加,但在类似的年径流中,LCR流域的年NO_3-N产量比SFIR少。这两个流域彼此相距150公里以内,并且具有相似的主要农业系统,但是气候和农作物投入的差异影响了养分输送的数量和时间。

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