TY - JOUR
T1 - Composition of characteristic soils on the raised atoll Bellona, Solomon Islands
AU - Borggaard, Ole K.
AU - Koch, Christian Bender
AU - Elberling, Bo
AU - Breuning-Madsen, Henrik
AU - Stemmerik, Lars
N1 - Funding Information:
The authors would like to thank the farmers of Bellona for their willingness to participate in the questionnaire survey and interviews, and extension officer Kendrick Tangoeha, the Solomon Islands Ministry of Agriculture extension officer in Bellona for valuable guidance during our stays. This research was part of the ‘Sustainable resource use or imminent collapse? Climate, livelihoods and production in the southwest Pacific’ or CLIP project of the Galathea 3 expedition under the auspices of the Danish Expedition Foundation. CLIP was carried out in collaboration between the University of Copenhagen, the Danish Meteorological Institute and Solomon Islands Meteorological Service Centre. We are grateful to the Danish Expedition Foundation for accepting the project and for ensuring funding from Bikubenfonden and for funding provided by Knud Højgaards Fond , COWIfonden , Brødrene Hartmann's Fond and the Department of Geography and Geology, University of Copenhagen .
PY - 2012/1/15
Y1 - 2012/1/15
N2 - Knowledge is scarce about the composition of soils on Bellona and other Pacific atolls. Such knowledge is important as it is closely related to sustainable land use of these special soils formed on carbonatic/phosphatic materials. Therefore, the micromorphological, chemical and mineralogical composition of samples from genetic horizons in three dominant Bellonese soils (Malanga, Kenge Ungi and Kenge Toaha) and underlying rock (Tanahu) were investigated. Tanahu mainly consists of dolomite, but this mineral is absent in the three soils, which are dominated by phosphate-containing minerals. The Malanga soil is strongly dominated by Ca and P with minor amounts of Al, F and Fe present in fluorapatite, hydroxyapatite and crandallite. In contrast, Al, Fe and P dominate in the Kenge Ungi and Kenge Toaha soils in accordance with a mineralogy consisting of crandallite together with aluminum oxides (gibbsite/boehmite) and iron oxides, mainly goethite with minor contents of hematite. The observed carbonate for phosphate substitution in the apatites and crandallite is important as it indicates an increased phosphate availability in the soils. All three soil samples contain ≤ 1% Si and very little K and Mg. Total contents of essential microelements are considered adequate, but the rather high contents of Sr and U, especially in the Kenge Ungi soil may be problematic. Although the composition of the soils suggests substantial fertility and resilience, the lack of K-containing weatherable minerals (silicate minerals) is in line with a very low K (and low Mg) content and explains why fertilization may be needed to sustain future cultivation of these special soils. Due to a possible low bioavailability of Fe, Mn and maybe other micronutrients at the circumneutral pH of these carbonatic/phosphatic soils as well as the rather high contents of Sr and U, it may be recommended to test element availability using appropriate chemical soil tests supplemented by plant experiments to ensure safe and sustainable (optimal) soil use. However, according to the local farmers, the Malanga, Kenge Toaha and Kenge Ungi soils are considered well suited for production of the preferred crops.
AB - Knowledge is scarce about the composition of soils on Bellona and other Pacific atolls. Such knowledge is important as it is closely related to sustainable land use of these special soils formed on carbonatic/phosphatic materials. Therefore, the micromorphological, chemical and mineralogical composition of samples from genetic horizons in three dominant Bellonese soils (Malanga, Kenge Ungi and Kenge Toaha) and underlying rock (Tanahu) were investigated. Tanahu mainly consists of dolomite, but this mineral is absent in the three soils, which are dominated by phosphate-containing minerals. The Malanga soil is strongly dominated by Ca and P with minor amounts of Al, F and Fe present in fluorapatite, hydroxyapatite and crandallite. In contrast, Al, Fe and P dominate in the Kenge Ungi and Kenge Toaha soils in accordance with a mineralogy consisting of crandallite together with aluminum oxides (gibbsite/boehmite) and iron oxides, mainly goethite with minor contents of hematite. The observed carbonate for phosphate substitution in the apatites and crandallite is important as it indicates an increased phosphate availability in the soils. All three soil samples contain ≤ 1% Si and very little K and Mg. Total contents of essential microelements are considered adequate, but the rather high contents of Sr and U, especially in the Kenge Ungi soil may be problematic. Although the composition of the soils suggests substantial fertility and resilience, the lack of K-containing weatherable minerals (silicate minerals) is in line with a very low K (and low Mg) content and explains why fertilization may be needed to sustain future cultivation of these special soils. Due to a possible low bioavailability of Fe, Mn and maybe other micronutrients at the circumneutral pH of these carbonatic/phosphatic soils as well as the rather high contents of Sr and U, it may be recommended to test element availability using appropriate chemical soil tests supplemented by plant experiments to ensure safe and sustainable (optimal) soil use. However, according to the local farmers, the Malanga, Kenge Toaha and Kenge Ungi soils are considered well suited for production of the preferred crops.
KW - Apatite
KW - Crandallite
KW - Dolomite
KW - Fertility
KW - Phosphate
KW - Resilience
UR - http://www.scopus.com/inward/record.url?scp=84155183009&partnerID=8YFLogxK
U2 - 10.1016/j.geoderma.2011.10.001
DO - 10.1016/j.geoderma.2011.10.001
M3 - Article
AN - SCOPUS:84155183009
SN - 0016-7061
VL - 170
SP - 186
EP - 194
JO - Geoderma
JF - Geoderma
ER -