Pedogenic Loss and Uptake of Calcium by Gmelina Growing in an Isohyperthermic Kandiudult
This study evaluated temporal soil calcium loss within the soil and uptake by plants using Gmelina arborea form 2002 to 2006 at a watershed in Owerri, Southeastern Nigeria Forty pedons were dug and sampled at a regular grid of 400x400 m while 10 Gmelina plants were marked and used for the temporal evaluation of calcium (Ca). Standard analyses were performed on both soil and plant samples. Data obtained were subjected to analysis of variance (ANOVA) and correlation analyses using standard computer software. Results showed significant (p<=0.05) differences in elemental ratios with depth and time. Leaf Ca also varied significantly (p = 0.05) temporally. There were significant positive correlations between soil and plant Ca in 2002 and 2003, non-significance in 2003 while significant negative correlations (p<0.0001) in 2005 and 2006.
Land degradation is a topical issue, especially in the lowland states of southeastern
Nigeria where soil erosion by the agency of water has dissected the landscape.
Igwe (2003) identified rainfall as a major component
contributing to land degradation. High rainfall amount and duration favour leaching
of soil nutrients including calcium from upper horizons to deeper part of the
pedon. This translocatory pedogenic loss via leaching was attributed to soil
aggregate instability (Igwe, 2000). These losses lead
to declining productivity of soils especially in arable agriculture as nutrients
are leached away from the rhizosphere. It was also reported (Jandl
et al., 2004) that deposition of large amounts of atmospheric sulphur
and nitrogen promoted loss of calcium in soils of central European forests.
The danger in calcium loss is that uptake of some other basic cations, such
as magnesium is retarded (Osemwota et al., 2003).
Despite the ability of trees to extend their taproots to deeper layers of soils,
calcium loss has been reported (Huntington, 2000) and
Ca deficiency (Rothe et al., 2002) showed by
plants due to insufficiency of soil exchangeable calcium.
The choice of Gmelina was due to its dominance and use for conservation of the Otamiri river. Gmelina arborea is a relatively fast growing tree when compared with most of the indigenous watershed plants. But it was observed that most other plant types associated with these Gmelina-dominated vegetation show a variety of deficiency symptoms. Remarkable deficiency symptoms are exhibited by arable crops cultivated under these trees after seasonal pruning. In line with the above, the study investigated vertical distribution of calcium in soils of Otamiri watershed and related the soil calcium concentration to calcium content of leaves of Gmelina arborea.
MATERIALS AND METHODS
The study site is part of Otamiri watershed in Imo State, southeastern Nigeria,
lying between latitudes 4°151 and 7°051 North
and longitudes 5°501 and 9°301 East. This investigation
was conducted from 2002 to 2006 although a reconnaissance part of the study
commenced in 2001 in the above watershed in Owerri, Imo State, Southeastern
Nigeria. It represents a 70 ha large, 30 year old Gmelina-dominated vegetation.
The geology is dominated by deeply weathered coastal plain sands (Benin formation)
of the Oligocene-Miocene era. The watershed is a typical humid environment.
The average precipitation in the area is 2500 mm with 3 distinct months of dryness,
while the average annual temperature ranges from 26-29°C. Soils of the study
site are very sandy and acidic and classified as isohyperthermic Kandiudults
(Soil Survey Staff, 2003) and correlated to FAO-classification
(FAO, 1998) as Dystric Nitisols. Riverside farming is
a major socio economic activity.
Since 2002 precipitation was sampled with 20 open thoroughfall collectors with a cross section area of 300 cm2. The thoroughfall collectors were arranged along a transect at a 2 m interval. Soil solutions were collected fortnightly from June 2001 at the study site at fixed sampling depths of 20 and 100 cm using ceramic suction Iysimetres at a tension of 40 KPa (P-80, Berliner Porzellanmanufaktur, Germany). Twenty replicate Iysimeters per sampling depth were installed, each located adjacent to a throughfall sampler. Forty pedons (soil profile pits) were dug and sampled along a regular grid of 400x400 m. Soil samples were collected from the bottommost pedogenic horizon based on pedogenetic differentiation. Soil samples from each pedon were analyzed individually. Exchangeable cations, namely calcium (Ca); magnesium (Mg), potassium (K), sodium (Na), manganese (Mn), aluminium (Al) and iron (Fe) were estimated by inductively coupled plasma atomic emission spectrometer (ICP-AES) (Integra XMP, GBC, Arlington Heights, IL). Base Saturation (BS) was computed as a sum of exchangeable basic cations divided by CEC (cation exchange capacity). The CEC was determined by percolating 2.5 g of soil with 100 mL of 1 m ammonium chloride for about 4 h. Before percolating the soil sample, samples were soaked with extraction solution overnight. Soil pH was measured using a glass electrode in deionized water (pHDDI) at a soil solution ratio of 1:2.5.
Water extractable sulphate was estimated by 5 sequential batch extractions of moist soil with distilled water at a soil: Solution ratio of 1:5 and sulphate in the extracts were measured by ion chromatography.
The vegetation of the site was dominated by Gmelina arborea, thus was used as indicator plant for the study. Leaves were sampled from the upper canopy at the end of the rainy season (October through November) for 2002, 2003, 2004, 2005 and 2006. Leaves from 10 trees were harvested each year, separated according to age and analyzed using composite mixed samples per leaf age and tree. The same tree stands were marked and used throughout the study. Leaf samples were milled after drying at 60°C and 100 mg was digested in 1 mL of 1 M HNO3 at a temperature of 170°C for cation analysis using ICP-AES.
Soil data were subjected to analysis of variance (ANOVA) and multiple comparison
of means for the experimental period was conducted using the procedure of GLM,
Duncan test). Individual statistical analysis of pedogenic horizons was done
and differences were considered significant at p<0.01. The temporal trend
of the Ca concentration in leaves Gmelina arborea was calculated as linear
regression (procedure REG). Differences between years were tested with a repeated
measures analysis of variance (procedure GLM, SAS Institute,
1989). A linear regression was used to relate soil and leaf data. Derived
equations were tested for significance by ANOVA with the statistics module of
Sigma Plot for Windows 2001 (SPSS Science, Chicago, IL).
RESULTS AND DISCUSSION
Results on soil chemical parameters are shown in Table 1.
Soil horizons were well-differentiated and very deep. Bulk density increased
with depth. Soils were strongly to moderately acidic while Cation Exchange Capacity
(CEC) was low and showed no defined trend in distribution.
|| Selected soil properties of the study site (mean values)
|BD = Bulk Density, CEC = Cation Exchange Capacity, BS = Base
Saturation, Alsat = Aluminium Saturation
|| Ratios of exchangeable cations in soils of the study site
|| Temporal variability in the distribution cationic ratios
|| Relationship between some measured parameters of soils with
time (n = 200)
|**: Significant at p = 0.01; *: Significant at p = 0.05; NS
= Not Significant
Results on CEC and pH are consistent with the findings of Onweremadu
et al. (2006a). Starting from the eluvial horizon, exchangeable calcium
increased with depth while exchangeable magnesium indicated an irregular trend.
Base Saturation (BS) increased with depth and the reverse was the case for aluminium
Elemental ratios were used as indicators to infer nutritional balance (Table
2). There were significant reductions (p = 0.05) in Ca/Mg and Ca+Mg/Al+H
ratios in the vertical distribution of these ratios. Significant (p = 0.0) variation
in horizon distribution was observed in Ca/Al ratios in the site. In a similar
study, Oti (2002) reported a consistent decrease in
Ca+Mg/Al+H ratio in the same region.
There were significant (p = 0.05) changes in elemental ratios with time
(Table 3). A statistically significant (p = 0.05) decrease
was observed during the period from 2002 to 2006 in all the elemental ratios
at pedon levels of analysis. With the exception of bulk density (BD), other
measured soil parameters had significant correlation with exchangeable calcium
(Table 4), especially NO3 and Alsat. Generally,
calcium concentration in leaves of Gmelina arborea declined consistently
with time (Table 5).
|| Temporal variability in elemental chemistry and sufficiency
ranking of Ca in levels of Gmelina asborea
|Ranking was adapted from the study of Bergmann
However, leaf Ca-concentration was above threshold limit (Bergman, 1992) for
2002 and 2003 years of plant life. Soil Ca had significant positive correlation
coefficients in 2002 and 2003 (p<0.05) but was statistically non-significant
in 2004 (Table 6). Conversely, there was significant negative
correlation between both parameters in 2005 and 2006 (Table 6).
Calcium loss in soils of study site was significant (p≤0.05) as concentrations
increased towards the deeper soil horizons. The losses were mainly from the
surface and eluvial layers. In the surface layers, plant litter decomposed to
release organic acids, such as fulvic acid which aid dissolution and consequent
mobility of basic cations including Ca. In the eluvial horizon, leaching losses
of soil Ca was permanent. Due to Ca loss, the Ca/Al ratio of E-horizon was least
in all the sampled pedons. Soils Ca loss could be attributed to low Ca input
and continued leaching of SO42¯ and NO3¯
(Likens et al., 1996). The E-horizons were also
associated with very high Alsat (mean = 75%), which implies high possibility
of aluminium toxicity. High levels of soluble Al concentrations in soils is
toxic to plants and becomes a serious productivity constraint when it reaches
60% or more (Styzcen, 1992). This may not be a serious
problem to Gmelina arborea since it is deeply rooted, suggesting that
the roots explore the illuvial Bt-horizons having high concentrations of soil
Ca and exchangeable Ca. But for shallow rooted crops, such as maize, which is
commonly grown in the watershed, performance may be low except when soil fertility
is augmented. This is due to the low Ca/Mg ratio (below 3.00) in the rhizosphere.
Earlier, Landon (1984) reported that Ca/Mg ratio below
3 results in the unavailability of Ca and phosphorus. Consistency in Ca/Mg,
Ca+Mg/Al+H and Ca/Al ratios is suggestive of using these elemental ratios as
indicators of degree of leaching losses in soil Ca in the humid tropics. Highly
significant correlations (p = 0.01) between soil Ca with NO3 and
Alsat (Table 4) is predictive of the abundance of soil Ca
and exchangeable Ca. Concentrations in leaf Ca decreased up to 2005 but increased
to 2.76 mg g-1 in 2006. This is possibly due to greater ability of
Gmelina taproot system to explore deeper horizons for nutrients, while it was
unable to trap the translocating soil Ca. It is also possible that Gmelina may
have derived part of its Ca-requirement by absorbing soil Ca released directly
from parent materials (Jandl et al., 2004). However,
association of Gmelina roots with mycorrhizal fungi could be beneficial to the
plant since these fungi dissolve Ca from Ca-feldspars (Blum
e tal., 2002). Although these Gmelina plants are having increasing leaf
Ca with decreasing soil Ca (Table 6), it is a worrisome trend
for arable crops and soil bacterial biomass which suffer soil acidification
(Bladodatskaya and Anderson, 1999) and this could be
why Onweremadu et al. (2006b) suggested the use
ground seashells as liming materials on Isohyperthermic Arenic Kandiudult.
The study showed that leaching is a major pedogenic process influencing the
distribution of soil calcium in the site. The Ca/Mg ratios were below 3.00 in
surface horizons, indicating their unsuitability for arable agriculture while
trees such as Gmelina with taproot system can extend roots to explore deeper
layers. As a result of consistency in the results of elemental ratios, they
could be used for predicting calcium abundance and exchangeability in the study
Grateful to Engr. Dr. Ezekiel Izuogu, for financial assistance in this study.
Bergmann, W., 1992.
Nutritional Disorders of Plants: Development, Visual and Analytical Diagnosis. G. Fischer, Jena, Germany
Bladodatskaya, E.V. and T.H. Anderson, 1999.
Adaptive responses of soil microbial communities under experimental acid stress in controlled laboratory studies. Applied Soil Ecol., 11: 207-216.Direct Link |
Blum, J.D., A. Klaue, C.A. Nezat, C.T. Driscoll and C.E. Johnson et al
Myccorrhizal weathering of apatite as an important calcium source in base-poor forest ecosystems. Nature, 417: 729-731.
World reference base for soil resources. World Soil Resources Reports of the Food and Agricultural Classification of the United Nations, Rome.
Huntington, G.T., 2000.
The potential of calcium sepletion in forest ecosystems of Southeastern United States: Review and analysis. Global Biogeochem. Cycles, 14: 623-638.Direct Link |
Igwe, C.A., 2000.
Nutrient losses in runoff and eroded sediments from spoils of central Eastern Nigeria. Polish Soil Sci., 33: 67-75.
Igwe, C.A., 2003.
Soil degradation response to soil factors in Central Eastern Nigeria. Proceedings of the 28th Annual Conference of Soil Science Society of Nigeria, November 4-7, 2003, Umudike Umuahia, Nigeria, pp: 228-234
Jandl, R., C. Alewell and J. Prietzel, 2004.
Calcium loss in Central European forest soils. Soil Sci. Soc. Am. J., 68: 588-595.Direct Link |
Landon, J.R., 1984.
Booker Tropical Manual: A Handbook for Soil Survey and Agricultural Land Evaluation in the Tropics and Subtropics. Longman, New York
Likens, G.E., C.T. Driscoll and D.C. Buso, 1996.
Long-term effects of acid rain: Response and recovery of a forest ecosystem. Science, 272: 244-246.Direct Link |
Onweremadu, E.U., C.C. Opara, U. Nkwopara, C.I. Duruigbo and I.I. Ibeawuchi, 2006.
Yield response of a cowpea variety on ground seashells on Isohyperthermic Kaudiudult of Owerri, Southeastern Nigeria. Int. J. Soil Sci., 3: 251-257.CrossRef | Direct Link |
Onweremadu, E.U., I.C. Okoli, O.O. Emenalom, M.N. Opara and E.T. Eshett, 2006.
Soil quality evaluation in rangeland soils in relation to heavy metals pollution. Estud. Biol., 28: 37-50.CrossRef | Direct Link |
Osemwota, I.O., J.A.I. Omueti and A.I. Ogbogbodo, 2003.
Effect of Ca/Mg, ratio in the soil on Mg availability, yield and yield components of maize (Zea mays
L.). Proceedings of the 28th Annual Conference of Soil Science Society of Nigeria Held at National Root Crop Research Institute, November 4-7, 2003, Umudike, Abia State Nigeria, pp: 91-98
Oti, N.N., 2002.
Discriminant functions for classifying erosion degraded lands at Otamiri, South eastern Nigeria
. Agron. Sci., 3: 34-40.CrossRef | Direct Link |
Rothe, A., C. Huber, K. Kreutzer and W. Weis, 2002.
Deposition and soil leading in stands of Norway Spruce and European beech: Results from the Hoglwald research in comparison with other European case studies. Plant Soil, 240: 33-45.Direct Link |
SAS for Windows, Version 6.10. SAS Institute, Cary, NC
SSS (Soil Survey Staff), 2003.
Keys to Soil Taxonomy. 9th Edn., United States Department of Agriculture, UK., pp: 263-284
Styzcen, M., 1992.
Effects of Erosion on Soils and Growing Periods in Nigeria. In: Erosion, Conservation and Small-Scale Farming, Hurni, H. and K. Tato (Eds.). Isco/Waswe Publisher, UK., pp: 582