Impact of soil and water conservation measuren on catchment hydrological response: a case in north Ethiopia

Impact studies of catchment management in the developing world rarely include detailed hydrological components. Here, changes in the hydrological response of a 200-ha catchment in north Ethiopia are investigated. The management included various soil and water conservation measures such as the construction of dry masonry stone bunds and check dams, the abandonment of post-harvest grazing, and the establishment of woody vegetation. Measurements at the catchment outlet indicated a runoff depth of 5 mm or a runoff coefficient (RC) of 1·6% in the rainy season of 2006. Combined with runoff measurements at plot scale, this allowed calculating the runoff curve number (CN) for various land uses and land management techniques. The pre-implementation runoff depth was then predicted using the CN values and a ponding adjustment factor, representing the abstraction of runoff induced by the 242 check dams in gullies. Using the 2006 rainfall depths, the runoff depth for the 2000 land management situation was predicted to be 26·5mm(RCD 8%), in line with current RCs of nearby catchments. Monitoring of the ground water level indicated a rise after catchment management. The yearly rise in water table after the onset of the rains (ΔT) relative to the water surplus (WS) over the same period increased between 2002-2003 (ΔT/WS D 3·4) and 2006 (ΔT/WS >11·1). Emerging wells and irrigation are other indicators for improved water supply in the managed catchment. Cropped fields in the gullies indicate that farmers are less frightened for the destructive effects of flash floods. Due to increased soil water content, the crop growing period is prolonged. It can be concluded that this catchment management has resulted in a higher infiltration rate and a reduction of direct runoff volume by 81% which has had a positive influence on the catchment water balance. © 2010 John Wiley & Sons, Ltd

Vanishing wildlife corridors and options for restoration: a case study from Tanzania

Conserving wildlife corridors is increasingly important for maintaining ecological and genetic connectivity in times of unprecedented habitat fragmentation. Documenting connectivity loss, assessing root causes, and exploring restoration options are therefore priority conservation goals. A 2009 nationwide assessment in Tanzania documented 31 major remaining corridors, the majority of which were described as threatened. The corridor between the Udzungwa Mountains and the Selous Game Reserve in south-central Tanzania, a major link between western and southern wildlife communities, especially for the African elephant Loxodonta africana, provides an illuminating case study. A preliminary assessment in 2005 found that connectivity was barely persisting via two remaining routes. Here we present assessments of these two corridors conducted from 2007-2010, using a combination of dung surveys, habitat mapping and questionnaires. We found that both corridor routes have become closed over the last five years. Increased farming and livestock keeping, associated with both local immigration and population growth, were the main reasons for corridor blockage. However, continued attempts by elephants to cross by both routes suggest that connectivity can be restored. This entails a process of harmonizing differing land owners and uses towards a common goal. We provide recommendations for restoring lost connectivity and discuss the prospects for preventing further loss of corridors across the country

Acid sulphate soil characterization in Negara Brunei Darussalam: a case study to inform management decisions

A diverse range of acid sulphate soils occur in Negara Brunei Darussalam on the inland flat areas that are important agricultural lands. Prior to this study, there was no information on their occurrence. Information about these soils is critical because they present significant management challenges for both agriculture and protection of the environment. Field surveys and laboratory analysis conducted in eight areas of the Brunei-Muara district and four areas of the Belait district identified, characterized and classified using Soil Taxonomy, a wide range of 10 acid sulphate soil types in four soil orders: Histosols, Vertisols, Inceptisols and Entisols. A user-friendly soil identification key using easily observed soil characteristics was developed to assist users with the recognition of the range of acid sulphate soils. Conceptual soil hydro-toposequence models in the form of cross-sections were constructed to explain the spatial heterogeneity of (i) acid sulphate soil properties comprising a range of features (e.g. organic-rich materials/peats, clays, sands, cracks and jarosite-rich mottles), sulphidic material and sulphuric horizons, (ii) pyrite shale outcrops and (iii) soil types using both the soil identification key and Soil Taxonomy. The soil hydro-toposequence models together with the soil identification key helped to easily visualize and illustrate the complexities and importance of understanding specific sites to assess the detailed behaviour and implications of various soil, regolith and topographic features. © 2013 British Society of Soil Science.G.J. Grealish & R.W. Fitzpatric