Potential phosphorus losses from grassland soils irrigated with dairy factory wastewater

被引:3
|
作者
Lizarralde, C. A. [1 ]
McDowell, R. W. [1 ,2 ]
Condron, L. M. [1 ]
Brown, J. N. [3 ]
机构
[1] Lincoln Univ, Fac Agr & Life Sci, POB 84, Christchurch 7647, New Zealand
[2] AgResearch, Lincoln Sci Ctr, Private Bag 4749, Christchurch 8140, New Zealand
[3] Fonterra Cooperat Grp, Fonterra Res & Dev Ctr, Private Bag 11029, Palmerston North 4442, New Zealand
关键词
Anion storage capacity; Effluent; Land application; Leaching; Surface runoff; NEW-ZEALAND; CHEMICAL AMENDMENTS; EFFLUENT; RUNOFF;
D O I
10.1007/s10705-021-10165-2
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Applying phosphorus (P)-rich wastewater to land can significantly enrich P in topsoil and consequently increase the risk of P losses in surface runoff and leaching. We collected 654 samples (0-7.5, 7.5-15, and 15-30 cm depths) of wastewater-irrigated and non-irrigated soils at seven sites across New Zealand to assess the potential P mobility in irrigated soils. The risk of P loss to surface runoff was tested by water extractable P (WEP) whereas the risk of P loss by leaching was tested by calcium chloride extractable P (CaCl2-P). These environmental P tests are rarely analysed; hence, a published relationship was used to determine if the risk of P losses could be predicted using anion storage capacity (ASC) and Olsen P, two agronomic tests used in New Zealand. The magnitude of WEP and CaCl2-P could be predicted using the published relationship, but only in non-irrigated soils. Additionally, the mixed model analysis that compared soils and irrigated treatments showed that wastewater-irrigated soils had a greater pH, WEP and CaCl2-P concentration to 30 cm depth. However, in both irrigated and non-irrigated soils a change point or threshold in ASC was found that could be used to show an increased likelihood of enhanced P leaching (as CaCl2-P) to deeper layers. In addition, the WEP and CaCl2-P thresholds, can be used to signal the need for management changes to decrease the risk of P losses to surface water and groundwater.
引用
收藏
页码:69 / 84
页数:16
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