[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
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The Valley Bottom soils have organic carbon cont<strong>en</strong>ts cont<strong>en</strong>ts <strong>of</strong> 2.5-6.5% 2.5-6.5% in <strong>the</strong> topsoils. The total<br />
nitrog<strong>en</strong> cont<strong>en</strong>ts <strong>of</strong> <strong>the</strong> topsoil are comparable with <strong>the</strong> o<strong>the</strong>r soils. The subsurface horizons<br />
show organic carbon and total nitrog<strong>en</strong> cont<strong>en</strong>ts similar to those <strong>of</strong> <strong>the</strong> Ebom and Ebimimbang<br />
soils.<br />
5.4.3 Available and total phosphorous<br />
The available phosphorous cont<strong>en</strong>t in <strong>the</strong> topsoils <strong>of</strong> <strong>the</strong> Nyangong soils ranges betwe<strong>en</strong> 4 and<br />
11 ppm (low), in <strong>the</strong> Ebom and Ebimimbang soils betwe<strong>en</strong> 10 and 26 ppm (moderate) and in <strong>the</strong><br />
Valley Bottom soils betwe<strong>en</strong> 30 and 60 ppm (moderate to high). With depth, available<br />
phosphorous cont<strong>en</strong>ts drop rapidly to values below 5 ppm and are invariably approaching 0 in<br />
all subsoils.<br />
Total phosphorous cont<strong>en</strong>ts <strong>of</strong> <strong>the</strong> topsoils are high in <strong>the</strong> Nyangong soils and range betwe<strong>en</strong><br />
400 and 600 ppm. With depth, <strong>the</strong>se values go down to 50-250 ppm. The Ebom and Ebimimbang<br />
soils have 150-400 ppm total phosphorous in <strong>the</strong> topsoils and 50-250 ppm in <strong>the</strong>ir subsoils. Total<br />
phosphorous cont<strong>en</strong>ts <strong>of</strong> <strong>the</strong> Valley Bottom soils are not available.<br />
Higher available phosphorous cont<strong>en</strong>ts coincide with higher pH values as at higher pH values<br />
phosphorous is less fixed in aluminium and iron complexes than at lower pH ranges. The higher<br />
available phosphorous cont<strong>en</strong>ts <strong>of</strong> <strong>the</strong> Valley Bottoms are explained by colluvial <strong>en</strong>richm<strong>en</strong>t.<br />
Table 5.4b 5.4b Ranges in some chemical chemical characteristics <strong>of</strong> <strong>the</strong> four soil types types in <strong>the</strong> TCP TCP research<br />
area<br />
Soil type Depth Depth K+ Mg++ Ca++ TEB Al+++ Al+++ ECEC ECEC CEC CEC BS<br />
(%)<br />
Nyangong 1 0.1-0.5 0.2-0.8 1-2 1.5-3.5 4-9 6-10 10-20 10-20<br />
2 0-0.1 0-0.5 0.2-0.6 0.5-1.2 2-6 5-7 6-9 5-15<br />
Ebom 1 0.1-0.9 0.4-1.6 0.5-4 2-5 0.5-6 4-9 12-25 10-50<br />
2 0-0.2 0-0.5 0-0.5 0.3-1 2-5 3-6 5-8 5-20<br />
Ebimimbang 1 0.1-0.7 0-1.5 1-8 3-7 0-3 3-10 4-12 50-100<br />
2 0-0.2 0-0.5 0-2 0.2-1.5 1-2.5 1.5-1 2-6 10-70<br />
Valley 0-0.5 0.3-1.5 0.5-4 4.5-6 0-3 5-7.5 7-17 15-50<br />
Bottom 2 0-0.1 0-0.2 0-0.5 0.5-0.8 0-1.5 0.5-2 1-8 20-40<br />
Soil depth: 1 = topsoil, g<strong>en</strong>erally 0-10 cm; 2 = subsurface horizon <strong>of</strong> about 20-60 cm depth. TEB = Total<br />
Exchangeable Bases. ECEC = Effective Cation Exchange Capacity. CEC = Cation Exchange Capacity. BS = Base<br />
Saturation. All values, except BS, in meq per 100 g.<br />
5.4.4 Cation exchange capacity and exchangeable bases<br />
The cation exchange capacities (CEC) <strong>of</strong> <strong>the</strong> topsoils in <strong>the</strong> study area are low to moderate with<br />
CEC values <strong>of</strong> 4-20 mellOO gr soil. With depth <strong>the</strong> CECs drop rapidly to low levels <strong>of</strong> 1 to 9<br />
me/lOO gr in <strong>the</strong> subsurface horizons to ev<strong>en</strong> lower levels in <strong>the</strong> subsoils. The relatively higher<br />
CEC values occur in <strong>the</strong> topsoils topsoils <strong>of</strong> <strong>the</strong> Nyangong Nyangong and Ebom soils and are betwe<strong>en</strong> betwe<strong>en</strong> 10 and 25<br />
mell me/lOO 00 g soil. These higher values are directly related to <strong>the</strong> higher organic matter levels <strong>of</strong><br />
<strong>the</strong>se soils.<br />
The exchange exchange complex complex is dominated dominated by aluminium aluminium (AI) and Al saturation saturation perc<strong>en</strong>tages perc<strong>en</strong>tages <strong>of</strong> 30 to<br />
80% are common. The highest saturation values occur in <strong>the</strong> soils with <strong>the</strong> lowest pH values,<br />
50