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CONTROLLING SOIL EROSION AND RUNOFF WITH POLYACRYLAMIDE AND PHOSPHOGYPSUM ON SUBTROPICAL SOIL

机译:亚热带土壤中聚丙烯酰胺和磷素对土壤侵蚀和径流的控制

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Sandy soil, prone to intense soil erosion, is used for agriculture in the subtropics of Brazil. This study was conducted to determine whether soil amendments are effective for conserving topsoil by preventing water-induced erosion on a Brazilian sandy Alfisol soil (coarse-loamy, mixed, thermic Typic Paleudalf). A programmable rainfall simulator was used at the experimental station of the Federal University of Santa Maria, in a newly harvested black oat ( Avena estrigosa L.) field that was moldboard plowed and disked twice. Plots were on bare tilled soil with 8% to 12% slopes. The soil treatments consisted of a single 5 Mg ha -1 surface application of byproduct phosphogypsum (PG), a single 20 kg ha -1 surface application of anionic polyacrylamide (PAM), a combined amendment (PAM+PG) with the same rates as above, and an unamended soil (control). Simulated rainfall average intensity was 25 mm h -1 with a 2 h duration. Sediment and runoff samples were collected at intervals during the experiment, and soil surface samples inside the plot were taken after the rain for surface crusting analysis. Total soil loss was significantly lower for the treatments than for the control and averaged 197, 278, 217, and 2181 kg ha -1 , respectively for PG, PAM, PAM+PG, and control treatments. PAM and PAM+PG had steady-state runoff rates significantly less than that of the control. All of the amendments reduced soil sediment erosion (average 90% reduction) more than final runoff (average 35% reduction). Using amendments to reduce precipitation-induced erosion is a possible alternative conservation practice in this region of the world
机译:沙质土壤易遭受严重的土壤侵蚀,在巴西的亚热带地区用于农业。进行这项研究是为了确定土壤改良剂是否能通过防止水对巴西沙质Alfisol土壤(粗壤土,混合土壤,热性Typic Paleudalf)的侵蚀而有效地保护表土。圣塔玛丽亚联邦大学的实验站在一个新收获的黑燕麦(Avena estrigosa L.)田间中使用可编程降雨模拟器,将其犁过刨板两次。地块在裸土上,坡度为8%至12%。土壤处理包括副产品磷石膏(PG)的单次5 Mg ha -1 表面处理,阴离子聚丙烯酰胺(PAM)的单次20 kg ha -1 表面处理,具有与上述相同比率的组合修正(PAM + PG)和未修正的土壤(对照)。模拟降雨的平均强度为25 mm h -1 ,持续2 h。在实验过程中每隔一段时间收集沉积物和径流样品,并在雨后采集样地内的土壤表面样品以进行表面结皮分析。 PG,PAM,PAM + PG和对照处理的总土壤流失率明显低于对照,分别为197、278、217和2181 kg ha -1 。 PAM和PAM + PG的稳态径流率显着低于对照。所有修正案都比最终径流(平均减少35%)减少了土壤沉积物侵蚀(平均减少90%)。在世界上这个地区,使用修正案减少降雨引起的侵蚀是一种可能的替代性保护做法。

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