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定期进行牧场翻耕和重新播种导致的土壤流失:土壤湿度在控制风险中的重要性。

Sediment loss in response to scheduled pasture ploughing and reseeding: The importance of soil moisture content in controlling risk.

作者信息

Pulley S, Collins A L

机构信息

Sustainable Agriculture Sciences, Rothamsted Research, North Wyke, Okehampton, Devon, EX20 2SB, UK.

出版信息

Soil Tillage Res. 2020 Oct;204:104746. doi: 10.1016/j.still.2020.104746.

Abstract

Soil water regimes have been shown to have important implications for the erosion risks associated with land management decisions. Despite this, there remains a paucity of information on soil moisture thresholds for farm management operations including the periodic ploughing and reseeding of improved pasture used for ruminant farming. Against this background, this study analysed sediment loss monitored on a heavily instrumented farm platform, in SW England, over four phases of ploughing and reseeding. Precipitation and sediment yields were highly variable between the ten different field scale catchments on the experimental platform after reseeds. Post-plough period rainfall ranged between 461-1121 mm and corresponding sediment yields between 0.20 - 3.13 t. ha yr. The post-plough and reseeding periods accounted for a very high proportion (mean 28.8 %) of monitored sediment fluxes over the study (2012-2019) despite only covering an average of 10.9 % of the 2002 days of flume monitoring. Post-plough sediment yields were highest (2.57 t. ha yr and 3.13 t. ha yr) when two catchments were ploughed in autumn months and soils were saturated. The yields for the same catchments after summer ploughing were far lower (0.72 t. hayrand 0.73 t. hayr). Thresholds of 35-38 % soil moisture were identified at which ploughing represented a highly elevated erosion risk. Whilst pinpointing thresholds for the clay loam soils with slowly permeable drainage in the study area, the results serve to illustrate the wider need for robust scientific data on soil moisture status to help guide the timing of farm management operations for improving production, to help reduce negative environmental consequences.

摘要

土壤水分状况已被证明对与土地管理决策相关的侵蚀风险具有重要影响。尽管如此,对于包括反刍动物养殖用改良牧场的定期耕作和重新播种在内的农场管理操作,关于土壤湿度阈值的信息仍然匮乏。在此背景下,本研究分析了在英格兰西南部一个配备大量仪器的农场平台上,在四个耕作和重新播种阶段监测到的沉积物流失情况。重新播种后,实验平台上十个不同田间尺度集水区的降水量和沉积物产量变化很大。耕作后的降雨范围在461 - 1121毫米之间,相应的沉积物产量在0.20 - 3.13吨/公顷·年之间。尽管在2002天的水槽监测中,耕作和重新播种期仅平均占10.9%,但在整个研究期间(2012 - 2019年),它们在监测到的沉积物通量中所占比例非常高(平均28.8%)。当两个集水区在秋季耕作且土壤饱和时,耕作后的沉积物产量最高(2.57吨/公顷·年和3.13吨/公顷·年)。夏季耕作后,相同集水区的产量则低得多(0.72吨/公顷·年和0.73吨/公顷·年)。确定了土壤湿度阈值为35 - 38%,此时耕作代表着极高的侵蚀风险。在确定研究区域内排水缓慢的粘壤土的阈值时,这些结果有助于说明更广泛地需要关于土壤湿度状况的可靠科学数据,以帮助指导农场管理操作的时间安排,从而提高产量并减少负面环境影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b5a/7441785/5afc18ee4669/gr1.jpg

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