首页> 外文期刊>Agricultural and Food Science >Phosphorus losses from a subdrained clayey soil as affected by cultivation practices
【24h】

Phosphorus losses from a subdrained clayey soil as affected by cultivation practices

机译:耕作方式对低排水粘土土壤中磷的损失

获取原文
       

摘要

Conservation tillage practices are included in the Finnish Agri-Environmental Program as phosphorus (P) loss control measures, but only few experiments have been performed to check their effectiveness in the local conditions. We studied surface and subsurface losses of P from a clayey underdrained field (Jokioinen/ Kotkanoja; Vertic Cambisol/Typic Cryaquept), with 2% mean slope, during two separate experimental periods. Primary tillage treatments of the first experimental period of three years were moldboard ploughing (to 20?–23 cm depth) vs. no autumn tillage (wintertime stubble). During the second experimental period of five years, the treatments were moldboard ploughing (20?–23 cm) vs. shallow (to 5?–8 cm) autumn tillage. The stubble treatment of the first experimental period produced higher dissolved reactive P (DRP) losses (104?–259 g ha?–1 yr?–1) than autumn ploughing (77?–96 g ha?–1 yr?–1), and equally high particulate P (PP) losses (mean 660, 235?–1300 g ha?–1 yr?–1). During the second experimental period, shallow autumn tillage produced 28% higher DRP losses (mean 120, 107?–136 g ha?–1 yr?–1) than ploughing (83?–117 g ha?–1 yr?–1) and 11% higher PP losses (mean 1090, 686?–1336 g ha?–1 yr?–1) than ploughing (783?–1253 g ha?–1 yr?–1). Surface runoff made up 28% and 16% of the total flow from the ploughed soil during the first and the second experimental period, respectively, as compared to 50% for the stubble and 44% for the shallow autumn tillage. Routing of flow between surface and subsurface pathways had a major influence on the P losses. In the relatively flat landscapes of the main agricultural areas of southern Finland, the potential for decreasing agricultural P losses by reduced tillage appears limited.;
机译:保护性耕作方法作为磷(P)损失控制措施已包括在芬兰农业环境计划中,但是仅进行了很少的实验来检查其在当地条件下的有效性。我们研究了在两个单独的实验期间,来自黏性土壤排水田(Jokioinen / Kotkanoja; Vertic Cambisol / Typic Cryaquept)的P的表面和地下损失,平均斜率为2%。在三年的第一个实验期中,主要的耕作方法是翻土翻耕(至20?–23 cm深度),而不进行秋耕(冬茬)。在五年的第二个实验期中,处理方式为mold草犁(20?-23厘米)与浅耕(至5?-8厘米)的秋季耕作。第一个实验阶段的残茬处理产生的溶态反应性P(DRP)损失(104?-259 g ha?-1年-1年)高于秋耕(77?-96 g ha?-1年-1年)。 ,以及同样高的颗粒P(PP)损失(平均660,235?-1300 g ha?-1年yr-1)。在第二个实验期间,秋季耕作比耕作(83?–117 g ha?-1年?-1)高出28%的DRP损失(平均120,107?–136 g ha?-1年?-1)。与翻耕(783?–1253 g ha?-1年?-1)相比,PP损失(平均1090,686?-1336 g ha?-1yr?-1)高11%。在第一和第二个实验期间,地表径流分别占耕地土壤总流量的28%和16%,而茬茬土壤为50%,秋季耕作土壤为44%。地表和地下路径之间的流动路径对P损失有重大影响。在芬兰南部主要农业地区相对平坦的景观中,通过减少耕作减少农业磷素损失的潜力似乎有限。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号