2012
DOI: 10.1007/s10342-012-0639-0
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Predicting depth translocation of base cations after forest liming: results from long-term experiments

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Cited by 18 publications
(21 citation statements)
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References 52 publications
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“…Liming generally increases Δ BS especially where a large reduction of base saturation occurs indicating an efficient mitigation of further soil acidification after liming. With regard to a different depth interval (0-90 cm) considered in this study, the effect size is comparable to the findings of Guckland et al (2012) for sites in northwest Germany, who found differences in base saturation of 20%, 5% and 3% for the depth intervals 0-10 cm, 10-20 cm and 20-40 cm of limed as compared to unlimed plots, respectively. A strong effect of organic layer carbon stocks on Ca and Mg retention and base saturation changes was also described by Guckland et al (2012).…”
Section: Base Saturationsupporting
confidence: 86%
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“…Liming generally increases Δ BS especially where a large reduction of base saturation occurs indicating an efficient mitigation of further soil acidification after liming. With regard to a different depth interval (0-90 cm) considered in this study, the effect size is comparable to the findings of Guckland et al (2012) for sites in northwest Germany, who found differences in base saturation of 20%, 5% and 3% for the depth intervals 0-10 cm, 10-20 cm and 20-40 cm of limed as compared to unlimed plots, respectively. A strong effect of organic layer carbon stocks on Ca and Mg retention and base saturation changes was also described by Guckland et al (2012).…”
Section: Base Saturationsupporting
confidence: 86%
“…With regard to a different depth interval (0-90 cm) considered in this study, the effect size is comparable to the findings of Guckland et al (2012) for sites in northwest Germany, who found differences in base saturation of 20%, 5% and 3% for the depth intervals 0-10 cm, 10-20 cm and 20-40 cm of limed as compared to unlimed plots, respectively. A strong effect of organic layer carbon stocks on Ca and Mg retention and base saturation changes was also described by Guckland et al (2012). In summary, model results suggest that Δ BS is mainly dependent on the soil pools of basic substances at NFSI I, which is modified with respect to liming and soil organic matter status.…”
Section: Base Saturationsupporting
confidence: 86%
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“…However, the applied P dosages stayed mostly undocumented, so their influence on foliar P content at NFSI II plots cannot be estimated. Results of other studies (von Wilpert 2003;Guckland et al 2011) have found no reaction of the foliar P content after liming. However, Kulhavý et al (2009) detected an increase of P in current-year needles of Norway spruce after liming, and Huber et al (2006) reported on lower P contents in 1-and 2-year-old needles of Norway spruce 20 years after liming.…”
Section: Range Of Normal Foliar S Nutrition [Mg G à1 ] Typementioning
confidence: 83%
“…El pH del suelo presentó un comportamiento ascendente con el incremento de las dosis de los dos ME (figura 2d), de forma similar a los resultados reportados por Guckland et al (2012). Así mismo, el suelo presentó resistencia al cambio de pH, comportamiento propio de suelos con altos contenidos de arcillas, óxidos e hidróxidos de aluminio, hierro y manganeso, los cuales le confieren al suelo un fuerte poder buffer (He, Liu, Zhang, Wang, Shi, Corpoica Cienc Tecnol Agropecuaria, Mosquera (Colombia), 18(3):…”
Section: Resultados Y Discusiónunclassified