首页> 外文期刊>Australian Journal of Soil Research >Effect of variable soil phosphorus on phosphorus concentrations in simulated surface runoff under intensive dairy pastures.
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Effect of variable soil phosphorus on phosphorus concentrations in simulated surface runoff under intensive dairy pastures.

机译:集约化牧草场下可变土壤磷对模拟地表径流中磷浓度的影响。

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Intensive dairy operations in Australia regularly apply P fertiliser to maintain productive pasture species. However, extractable soil test P (STP) concentrations in this industry commonly exceed those required to maximise pasture production, a situation which can increase the risk of P loss to surrounding waterways. The current study examined relationships between STP (Olsen P and CaCl2 P) and surface runoff P concentrations from a red silty loam (Ferrosol), commonly used for pasture production in south-eastern Australia. Soil was mixed and re-packed into soil trays and a rainfall simulator was used to generate surface runoff. A wide range of soil Olsen P concentrations (0-20 mm, 15-724 mg/kg; 0-100 mm, 9-166 mg/kg) was created by surface-applying a range of P fertiliser rates 8 months before the rainfall simulations. A comparison of the 2 STP methods suggests that Australian soils have higher labile P concentrations for given Olsen P concentrations compared with those measured internationally, suggesting a greater likelihood of P loss in runoff. Furthermore, significant curvilinear relationships between STP and dissolved reactive P (DRP<0.45 micro m) in surface runoff for both Olsen P depths (0-20 mm, r2=0.94; 0-100 mm, r2=0.91; P<0.01) were determined, as well as significant linear relationships between DRP and both CaCl2 depths (0-20 mm, r2=0.83; 0-100 mm, r2=0.92; P<0.01). This confirmed that the concentrations of P in surface runoff increased with increasing STP, providing further evidence of an urgent need to reduce excessive STP concentrations, to reduce the risk of P loss to the environment.
机译:澳大利亚的集约化奶牛场定期使用磷肥来维持高产牧场种类。但是,该行业中可提取的土壤测试P(STP)浓度通常超过使牧草产量最大化所需的浓度,这种情况会增加P损失到周围水道的风险。目前的研究检查了STP(Olsen P和CaCl 2 P)与红色粉质壤土(Ferrosol)中地表径流P浓度之间的关系,该粉质壤土通常用于澳大利亚东南部的牧场生产。将土壤混合并重新包装到土壤盘中,并使用降雨模拟器产生地表径流。通过在降雨前8个月对磷肥的施用量进行表面处理,可产生多种土壤Olsen P浓度(0-20 mm,15-724 mg / kg; 0-100 mm,9-166 mg / kg)模拟。两种STP方法的比较表明,在给定的Olsen P浓度下,澳大利亚土壤比国际上测量的土壤具有更高的不稳定P浓度,这表明径流中P损失的可能性更大。此外,对于两种Olsen P深度(0-20 mm, r 2 = 0.94),地表径流中STP与溶解的反应性P(DRP <0.45 microm)之间存在显着的曲线关系。 ;确定0-100 mm, r 2 = 0.91; P <0.01),以及DRP和两个CaCl之间的显着线性关系 2 深度(0-20 mm, r 2 = 0.83; 0-100 mm, r 2 = 0.92; P <0.01)。这证实了地表径流中P的浓度随STP的增加而增加,进一步证明了迫切需要减少过量的STP浓度,以减少P损失到环境中的风险。

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