ESTIMATING SUBSOIL RESISTANCE TO NITRATE LEACHING FROM EASILY MEASURABLE PEDOLOGICAL PROPERTIES

被引:6
作者
Nakagawa, Fabio Keiti [1 ]
Siqueira Forti, Gabriel Benjamin [1 ]
Alves, Marcelo Eduardo [2 ]
Lavorenti, Arquimedes
de Miranda, Jarbas Honorio [3 ]
机构
[1] ESALQ USP, Escola Super Agr Luiz de Queiroz, BR-13418900 Piracicaba, SP, Brazil
[2] ESALQ USP, Dept Ciencias Exatas, BR-13418900 Piracicaba, SP, Brazil
[3] ESALQ USP, Dept Engn Biossistemas, BR-13418900 Piracicaba, SP, Brazil
来源
REVISTA BRASILEIRA DE CIENCIA DO SOLO | 2012年 / 36卷 / 05期
关键词
anion exchange capacity; remaining phosphorus; retardation factor; SPECTROPHOTOMETRIC DETERMINATION; REMAINING PHOSPHORUS; PHOSPHATE; SOILS;
D O I
10.1590/S0100-06832012000500013
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Leaching of nitrate (NO3-) can increase the groundwater concentration of this anion and reduce the agronomical effectiveness of nitrogen fertilizers. The main soil property inversely related to NO3- leaching is the anion exchange capacity (AEC), whose determination is however too time-consuming for being carried out in soil testing laboratories. For this reason, this study evaluated if more easily measurable soil properties could be used to estimate the resistance of subsoils to NO3- leaching. Samples from the subsurface layer (20-40 cm) of 24 representative soils of Sao Paulo State were characterized for particle-size distribution and for chemical and electrochemical properties. The subsoil content of adsorbed NO3- was calculated from the difference between the NO3- contents extracted with 1 mol L-1 KCl and with water; furthermore, NO3- leaching was studied in miscible displacement experiments. The results of both adsorption and leaching experiments were consistent with the well-known role exerted by AEC on the nitrate behavior in weathered soils. Multiple regression analysis indicated that in subsoils with (i) low values of remaining phosphorus (Prem), (ii) low soil pH values measured in water (pH H2O), and (iii) high pH values measured in 1 moL L-1 KCl (pH KCl), the amounts of surface positive charges tend to be greater. For this reason, NO3- leaching tends to be slower in these subsoils, even under saturated flow condition.
引用
收藏
页码:1491 / 1498
页数:8
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