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The limited availability of phosphate (Pi) in most soils results in the manifestation of Pi starvation responses in plants.
Gypsum content in agricultural soils results in restricted water and nutrient retention and the potential for dissolution piping, primarily in response to irrigation.
Heavy metal stress in soils results in subtle changes in leaf chlorophyll concentration, which are related to crop growth and crop yield.
As described by Paul [38] and Segers [39], microbial production of CH4 in soils results from the action of methanogen microorganisms that decompose organic material in the absence of O2, using CO2 as an electron acceptor and a reduced organic compound as the donor.
In addition, its rapid hydrolysis in soils results in a great quantity of nitrogen (30 50 %) running off and only a fraction is really absorbed by plants (Salman 1988; Malhi et al. 2001; Devassine et al. 2002; Ni et al. 2009; Da Rosa and dos Santos Rocha 2010).
Although phytoremediation has the potential for remediation of contaminated soils, results from both modeling and field studies suggested that plants may not always enhance the remediation efficiency when the soil already has a high microbial concentration, when the contaminant bioavailability is low, or when the overall reaction is mass transfer-limited.
Similar(52)
Podzolic soils (ash-gray forest soils), resulting from the cold of the long winter season, are found in the highlands.
Wetter soils resulted in vulnerability to compaction during planting and spraying operations.
The cumulative C mineralized increased in the sole manure and biochar amended soils, resulting in 45 125% positive PE.
On slope terrains, the downslope movement (creep) of active layer soils resulted in considerable CFS of tower foundations.
Heavy metal contamination of soils resulting from mining and smelting is causing major concern due to the potential risk involved.
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