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1 c denitrification in six soils (alkaline vs. acid soils).
2 re impediment to production of many crops in acid soil.
3 bserved low net nitrification rates in these acid soils.
4 ification rates are often low in subtropical acid soils.
5 Cassava Bacterial Blight (CBB), drought, and acid soils.
6 so be useful for capture of K, Ca, and Mg in acid soils.
9 (P < 0.05) compared to PT0 for rice paddies, acid soils, and the first 5 years of the experiments, re
10 cium (Ca), and magnesium (Mg) efficiency for acid soils; and (3) iron (Fe) and zinc (Zn) efficiency f
11 nts in hydroponic solutions and in naturally acid soil corresponded with their patterns of organic ac
14 The beneficial effect of FeP over TSP in the acid soil is attributed to the slow release of P from Fe
16 absence of net nitrification in some highly acid soils may be due to high rates of NO3(-)-N immobili
17 ere is an abrupt transition from alkaline to acid soil pH that occurs at the point where mean annual
18 verely limiting agricultural productivity in acid-soil regions comprising upwards of 50% of the world
19 h is caused by the solubilization of Al3+ in acid soils resulting in inhibition of root growth and nu
21 ajor limiting factors for crop production on acid soils that comprise significant portions of the wor
22 s, and enabling future molecular breeding of acid-soil-tolerant crops and trees, with huge potential
23 is a major constraint for crop production on acid soils which compose approximately 40% of arable lan
25 he primary limitation for crop production on acid soils, which make up 50% of the world's potentially