Soil Analysis

Sample taken from Canavà
Google Earth 44° 37’ 59.45” N 7° 56’38.88” E – Altitude: 286 m above sea level
Analysis carried out by Studio Tecnico Gribaudo Per. Agr. Giorgio – Turin

The western slope of La Morra is made up of Sant’Agata Fossil Marl, a blue-grey marl formed as sediment between 11 and 7 million years ago, during the Tortonian age. This was the fifth of the six stratification stages during the Miocene Epoch, the oldest geological epoch of the Neogene Period, which is the second period of the Cenozoic Era.

The composition of Rocche dell’Annunziata varies according to the parcel analysed: in the lower part of the valley, approaching Cannubi and the Diano Sandstone of Castiglione Falletto, sand predominates, whereas, as the slope rises (where Canavà is located) the texture of the soil becomes loamy, with a slight prevalence of sand over clay and in general a large quantity of lime, material that has the largest granules of clay. The plasticity index is 109 and therefore the soil is highly plastic, which is to say capable of handling and retaining a large maount of water.

grafici-terreno

tabella-analisi-1

Chemical composition Results
pH in H2O 8,338
pH in Kcl 7,434
Salinity 1:2 363
Salinity Saturation Extract 1140,63
Organic Carbon 0,813
Organic Substances 1,402
Ratio C/N 4,57
Base Saturation Degree 51,01
Ca/Mg 131,36
Mg/k 0,02
K/Mg 43,67
Chlorinating power index 3273,7
Mineralisation coeffecient 1,31
Cation exchange capacity 27,5
Ca+ 84,54
Mg+ 1,06
K+ 14,4
Total Calcium 15
Active Calcium 6,74
Total Nitrogen 0,178
Assimilable Phosphorus 20,886
Exchangeable Potassium 789,925
Exchangeable Magnesium 18,09
Exchangeable Calcium 2376,26
Assimilable Iron 19,061
Apparent Density 1,34
Apparent drying point 0,14
Equivalent humidity 34,77
Saturation 0,493
Hydraulic conductivity at saturation 0,77
Available water 198,72