Light acidification in N-fertilized loess soils along a climosequence affected chemical and mineralogical properties in the short-term

被引:14
作者
Antonela Iturri, Laura [1 ,2 ,3 ]
Eduardo Buschiazzo, Daniel [4 ,5 ]
机构
[1] Natl Univ La Pampa, CONICET UNLPam, Natl Council Res & Technol INCITAP, Inst Earth & Environm Sci La Pampa, Cc 186, RA-6300 Santa Rosa, Argentina
[2] Natl Univ La Pampa, Fac Agron, Cc 186, RA-6300 Santa Rosa, Argentina
[3] Natl Univ La Pampa, Fac Nat Sci, Cc 186, RA-6300 Santa Rosa, Argentina
[4] Natl Univ La Pampa, Anguil Expt Stn, Fac Agron, Natl Inst Agr Technol INTA, Cc 300, RA-6300 Santa Rosa, Argentina
[5] CONICET UNLPam, Natl Council Res & Technol INCITAP, Inst Earth & Environm Sci La Pampa, Cc 300, RA-6300 Santa Rosa, Argentina
关键词
N-fertilization; Short-term soil acidification; Loess soils; Soil buffer capacity; Climosequence; CATION-EXCHANGE CAPACITY; CLAY MINERALOGY; ACID; FORMS; AL;
D O I
10.1016/j.catena.2015.12.007
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Some evidences indicate that N-fertilization of crops decreased pH values of loess soils of the Argentinean Pampas in the last decades. We analyzed the A-horizons of four N-fertilized (F) and non-fertilized (NF) paired soils, developed on similar parent materials, within a climatic sequence (ustic to udic water regimes), and measured: 1) the extent of pH changes, 2) how these changes affected chemical and mineralogical soil properties and 3) how the soils, according to their H+ buffering substances, can react in the future if N-fertilization and acidification continue. Results indicated that all F- and NF soils were lightly acidified (differences between pH(W) and pH(KCl) higher than 1.0) and that fertilization produced pH decreases in all studied soils, but particularly in those with udic water regimes, in agreement with their longer N-fertilization histories. Fertilized ustic soils showed less crystalline illites and kaolinites and higher contents of amorphous Al oxides than NF soils. It remains unclear if the higher contents of amorphous Al are related with the dissolution of phyllosilicates, the transformation of the abundant volcanic glasses of these soils or both processes at the same time. The cation exchange capacity (CEC) and the percent of base saturation (V) did not change between F- and NF soils, probably due to the large influence of soil organic matter (SOM) in the studied soils. If N-fertilization, and consequently pH decreases continue, soils placed in both the moistest- (Argiudolls) and the driest extremes of the climosequence (Haplustolls) would be the less affected. This is because udic soils contain high SOM as well as illitic clays and silts while ustic soils contain free lime and high density charged clay minerals, which have high H+ neutralization capacity. The most affected soils by acidification should be those placed in the intermediate zone of the climosequence (Hapludolls), which have low amounts of substances with high buffer capacity. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:92 / 98
页数:7
相关论文
共 48 条
  • [1] [Anonymous], 1982, AGRONOMY MONOGRAPH 2, DOI DOI 10.2134/AGRONMONOGR9.2.2ED.C14
  • [2] Effect of land use and topography on soil properties and agronomic productivity on calcareous soils of a semiarid region, Iran
    Asadi, H.
    Raeisvandi, A.
    Rabiei, B.
    Ghadiri, H.
    [J]. LAND DEGRADATION & DEVELOPMENT, 2012, 23 (05) : 496 - 504
  • [3] How element translocation by plants may stabilize illitic clays in the surface of temperate soils
    Barre, P.
    Berger, G.
    Velde, B.
    [J]. GEODERMA, 2009, 151 (1-2) : 22 - 30
  • [4] Factors controlling spatial distribution of soil acidification and Al forms in forest soils
    Boruvka, L
    Mladkova, L
    Drabek, O
    [J]. JOURNAL OF INORGANIC BIOCHEMISTRY, 2005, 99 (09) : 1796 - 1806
  • [5] Brown G, 1984, In crystal structure of clay minerals and their identification, V5, P305
  • [6] Buschiazzo D. E., 1993, Ciencia del Suelo, V10/11, P46
  • [7] Buschiazzo D. E., 1988, Ciencia del Suelo, V6, P44
  • [8] Land use change in a temperate grassland soil: Afforestation effects on chemical properties and their ecological and mineralogical implications
    Cespedes-Payret, Carlos
    Pineiro, Gustavo
    Gutierrez, Ofelia
    Panario, Daniel
    [J]. SCIENCE OF THE TOTAL ENVIRONMENT, 2012, 438 : 549 - 557
  • [9] DARUSMAN, 1991, SOIL SCI SOC AM J, V55, P1097, DOI 10.2136/sssaj1991.03615995005500040034x
  • [10] Di Rienzo J.A., 2002, INFOSTAT PROFESSIONA