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  2. Soil acidification - Wikipedia

    en.wikipedia.org/wiki/Soil_acidification

    Aluminum is one of the few elements capable of making soil more acidic. [22] This is achieved by aluminum taking hydroxide ions out of water, leaving hydrogen ions behind. [23] As a result, the soil is more acidic, which makes it unlivable for many plants. Another consequence of aluminum in soils is aluminum toxicity, which inhibits root growth ...

  3. Metal ions in aqueous solution - Wikipedia

    en.wikipedia.org/wiki/Metal_ions_in_aqueous_solution

    A metal ion in aqueous solution or aqua ion is a cation, dissolved in water, of chemical formula [M(H 2 O) n] z+.The solvation number, n, determined by a variety of experimental methods is 4 for Li + and Be 2+ and 6 for most elements in periods 3 and 4 of the periodic table.

  4. Ionic strength - Wikipedia

    en.wikipedia.org/wiki/Ionic_strength

    The molar ionic strength, I, of a solution is a function of the concentration of all ions present in that solution. [3]= = where one half is because we are including both cations and anions, c i is the molar concentration of ion i (M, mol/L), z i is the charge number of that ion, and the sum is taken over all ions in the solution.

  5. Soil pH - Wikipedia

    en.wikipedia.org/wiki/Soil_pH

    Soil pH is a measure of the acidity or basicity (alkalinity) of a soil. Soil pH is a key characteristic that can be used to make informative analysis both qualitative and quantitatively regarding soil characteristics. [1] pH is defined as the negative logarithm (base 10) of the activity of hydronium ions (H + or, more precisely, H 3 O + aq) in ...

  6. Cation-exchange capacity - Wikipedia

    en.wikipedia.org/wiki/Cation-exchange_capacity

    Cation-exchange capacity (CEC) is a measure of how many cations can be retained on soil particle surfaces. [1] Negative charges on the surfaces of soil particles bind positively-charged atoms or molecules (cations), but allow these to exchange with other positively charged particles in the surrounding soil water. [2]

  7. Soil matrix - Wikipedia

    en.wikipedia.org/wiki/Soil_matrix

    It has two planes of silicon, one of aluminium and one of magnesium; hence it is a 2:2 clay. [43] Chlorite does not swell and it has low CEC. [41] [44] Kaolinite is a very common, highly weathered clay, and more common than montmorillonite in acid soils. [45] It has one silica and one alumina plane per crystal; hence it is a 1:1 type clay.

  8. Standard state - Wikipedia

    en.wikipedia.org/wiki/Standard_state

    The standard state molality is 1 mol/kg, while the standard state molarity is 1 mol/dm 3. Other choices are possible. For example, the use of a standard state concentration of 10 −7 mol/L for the hydrogen ion in a real, aqueous solution is common in the field of biochemistry.

  9. Equivalent concentration - Wikipedia

    en.wikipedia.org/wiki/Equivalent_concentration

    Since only 0.5 mol of H 2 SO 4 are needed to neutralize 1 mol of OH −, the equivalence factor is: f eq (H 2 SO 4) = 0.5. If the concentration of a sulfuric acid solution is c(H 2 SO 4) = 1 mol/L, then its normality is 2 N. It can also be called a "2 normal" solution.