TY - JOUR
T1 - Assessment of soil degradation and chemical compositions in Rwandan tea-growing areas
AU - Mupenzi, Jean De La Paix
AU - Li, Lanhai
AU - Ge, Jiwen
AU - Varenyam, Achal
AU - Habiyaremye, Gabriel
AU - Theoneste, Nzayisenga
AU - Emmanuel, Kamanzi
N1 - Funding Information:
This study was financially supported by the State Key Development Program for Basic Research of China (973 program, Grant No. 2010CB951002 ) and the Knowledge Innovation Project of Chinese Academy of Science ( KZCX2–YW–334 ). The authors would like to thank the Government of Rwanda, Rwanda National University, and China University of Geosciences (Wuhan/and Beijing) for adeptness and laboratory work. Many thanks to Prof. Y. Wang, President of China University of Geosciences, Mr. Hongtao Su and the editor for their helpful comments, advices and suggestions.
PY - 2011/12
Y1 - 2011/12
N2 - This study has focused on the processes of soil degradation and chemical element concentration in tea-growing regions of Rwanda, Africa. Soil degradation accelerated by erosion is caused not only by topography but also by human activities. This soil degradation involves both the physical loss and reduction in the amount of topsoil associated with nutrient decline. Soil samples were collected from eleven tropical zones in Rwanda and from variable depth within each collecting site. Of these, Samples from three locations in each zone were analyzed in the laboratory, with the result that the pH of all soil samples is shown to be less than 5 (pH < 5) with a general average of 4.4. The elements such as iron (Fe), copper (Cu), manganese (Mn), and zinc (Zn) are present in high concentration levels. In contrast calcium (Ca) and sodium (Na) are present at low-level concentrations and carbon (C) was found in minimal concentrations. In addition, elements derived from fertilizers, such as nitrogen (N), phosphorous (P), and potassium (K) which is also from minerals such as feldspar, are also present in low-level concentrations. The results indicate that the soil in certain Rwandan tea plantations is acidic and that this level of pH may help explain, in addition to natural factors, the deficiency of some elements such as Ca, Mg, P and N. The use of chemical fertilizers, land use system and the location of fields relative to household plots are also considered to help explain why tea plantation soils are typically degraded.
AB - This study has focused on the processes of soil degradation and chemical element concentration in tea-growing regions of Rwanda, Africa. Soil degradation accelerated by erosion is caused not only by topography but also by human activities. This soil degradation involves both the physical loss and reduction in the amount of topsoil associated with nutrient decline. Soil samples were collected from eleven tropical zones in Rwanda and from variable depth within each collecting site. Of these, Samples from three locations in each zone were analyzed in the laboratory, with the result that the pH of all soil samples is shown to be less than 5 (pH < 5) with a general average of 4.4. The elements such as iron (Fe), copper (Cu), manganese (Mn), and zinc (Zn) are present in high concentration levels. In contrast calcium (Ca) and sodium (Na) are present at low-level concentrations and carbon (C) was found in minimal concentrations. In addition, elements derived from fertilizers, such as nitrogen (N), phosphorous (P), and potassium (K) which is also from minerals such as feldspar, are also present in low-level concentrations. The results indicate that the soil in certain Rwandan tea plantations is acidic and that this level of pH may help explain, in addition to natural factors, the deficiency of some elements such as Ca, Mg, P and N. The use of chemical fertilizers, land use system and the location of fields relative to household plots are also considered to help explain why tea plantation soils are typically degraded.
KW - Chemical elements
KW - Fertilizer use
KW - Soil degradation
KW - Tea plantations
KW - pH
UR - http://www.scopus.com/inward/record.url?scp=80255131334&partnerID=8YFLogxK
U2 - 10.1016/j.gsf.2011.05.003
DO - 10.1016/j.gsf.2011.05.003
M3 - 文章
AN - SCOPUS:80255131334
SN - 1674-9871
VL - 2
SP - 599
EP - 607
JO - Geoscience Frontiers
JF - Geoscience Frontiers
IS - 4
ER -