In a glasshouse experiment, growth of C. vitalba increased with increasing rate of lime (CaCO3) and with increasing rate of applied P. Greatest growth in these conditions was associated with: pH = 4.7; exchangeable Al = 4.6 me./100 g; 0.02M CaCl2-extractable Al = 3.5 mg/g; and Olsen P = 56 mg/g. Death of plants was associated with: pH = 3.7; exchangeable Al = 12.6 me./100 g; 0.02M CaCl2-extractable Al = 107 mg/g; and Olsen P = 5.0 mg/g. The response to lime was to high pH and/or low Al concentrations rather than to high concentrations of Ca, indicating that C. vitalba is not a calcicole. Plant growth was found to be more closely correlated with CaCl2-extractable Al concentrations than to pH or exchangeable Al concentrations. In a second (subtractive nutrient) experiment, growth of C. vitalba was reduced by low concentrations of soil N, P, Ca, S, and micronutrients. The depression in growth in the minus micronutrient treatment appeared to be caused by low plant Mn concentrations, or possibly by high Fe concentrations as a result of the lower Mn concentrations. Despite very low concentrations of K and Mg in the soil, significant growth responses to the addition of these elements were not obtained. The addition of Fe was found to depress root growth.
The growth and spread of C. vitalba may be restricted by extremely acid soil conditions and by very low concentrations of N, P, Ca, S, and possibly Mn in the soil. However, it does not appear to be unusually sensitive to soil acidity or nutrient deficiencies.
Keywords Clematis vitalba; old man's beard; pH; soil nutrients; growth
New Zealand Journal of Botany, 1995, Vol. 33: 301-313
0028-825X/95/3303-0301 $2.50/0 (c) The Royal Society of New Zealand 1995
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