首页> 外文期刊>Soil Science Society of America Journal >Soil Nutrients and Other Major Properties in Grassland Fertilized with Nitrogen and Phosphorus
【24h】

Soil Nutrients and Other Major Properties in Grassland Fertilized with Nitrogen and Phosphorus

机译:氮磷配施的草地土壤养分及其他主要特性

获取原文
获取原文并翻译 | 示例
       

摘要

Understanding how nutrient distribution relates to soil depth is essential for improving fertilization practices for grasslands. This study evaluated the distribution of P, other elements, and selected soil properties at 0- to 5-cm and 5- to 15-cm layers in a grass sward following several years of N and P fertilization. Soil samples were collected in the spring of 2010 from a timothy grass sward (Phleum pratense L.) established in 1998 on a gravely-sandy loam soil. Sixteen combinations of P (0, 15, 30, and 45 kg ha(-1)) as triple superphosphate and N (0, 60, 120, and 180 kg ha(-1)) as calcic ammonium nitrate were broadcast annually from 1999 to 2006 in a split-plot design with P as main plots and N as subplots. Concentration of three soil P indicators [ water (C-P), Mehlich-3 (P-M3), and acid oxalate (P-Ox) extractable P] and total phosphorus (P-T) were greater in the 0- to 5-cm than in the 5- to 15-cm layer. Differences in concentration of C-P, P-M3, P-Ox, and P-T between the two soil layers increased with increasing P applications. The NH4OAc extractable Ca and Mg concentrations were significantly greater in the 0- to 5-cm soil layer compared with the 5- to 15-cm soil layer. The NH4OAc extractable K was significantly decreased by N application being greater in the 5- to 15-cm soil layer than in the 0- to 5-cm soil layer. Soil pH decreased and the concentration of Mehlich-3 Al increased with increasing N applications only in the 0- to 5-cm layer. This study demonstrated that several years of P fertilizer in grasslands could increase soil available P in the 0- to 5-cm layer, possibly due to lack of mixing and the low mobility of P. Our results also suggest that changes in soil chemical properties induced by N fertilizer in grasslands could be heightened at the 0- to 5-cm layer.
机译:了解养分分布与土壤深度之间的关系对于改善草原的施肥方法至关重要。这项研究评估了N和P施肥数年后草草中0至5 cm和5至15 cm层的磷,其他元素的分布以及选定的土壤性质。于2010年春季,从1998年在严重沙质壤土上的蒂莫西草皮草(Phleum pratense L.)收集了土壤样品。从1999年开始,每年广播十六种P(0、15、30和45 kg ha(-1))为三重过磷酸钙和N(0、60、120和180 kg ha(-1))为硝酸钙钙的广播。到2006年,采用分图设计,其中P为主要图,N为子图。 0至5 cm处的3种土壤P指标的浓度(水(CP),Mehlich-3(P-M3)和酸性草酸(P-Ox)可提取P)和总磷(PT)均大于对照。 5至15厘米的层。两种土壤层之间的C-P,P-M3,P-Ox和P-T浓度差异随P施用量的增加而增加。与5至15厘米土壤层相比,0至5厘米土壤层中NH4OAc可提取的Ca和Mg浓度明显更高。由于施氮量在5到15厘米土壤层中比在0到5厘米土壤层中更大,因此NH4OAc可萃取钾显着降低。仅在0至5 cm的土壤层中,土壤pH降低,Mehlich-3 Al的浓度随氮肥的施用而增加。这项研究表明,草原上的磷肥使用数年可能会增加0至5厘米层土壤速效磷,这可能是由于缺乏混合和磷的迁移率低所致。在0至5厘米的土壤层上,氮肥的施用量可以增加。

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