Application of a RUSLE-based soil erosion modelling on Mauritius Island

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  • Application of a RUSLE-based soil erosion modellingon Mauritius Island

    Rody NigelA,C and Soonil D. D. V. RughooputhB

    AStagiaire Postdoctoral, Bureau 5310, INRS Centre Eau Terre Environnement, 490 rue de la Couronne,Qubec, QC G1K 9A9, Canada.

    BFaculty of Science, University of Mauritius, Rduit, Mauritius.CCorresponding author. Email: Rody.Nigel@ete.inrs.ca

    Abstract. Soil erosion by water is one of the most important natural resources management problems in the world. Thedamages it causes on-site are soil loss, breakdown of soil structure, and decline in organic matter content, nutrient content,fertility, and inltration rate. Lands with the highest erosion risk on Mauritius Island are crop cultivations (sugarcane, tea,vegetables) on erosion-susceptible terrain (slopes >20% coupled with highly erodible soils). The locations of such lands onMauritius were mapped during previous, qualitatively based regional-scale erosion studies. In order to propose soilconservation strategies, there is a need to apply a more quantitative approach to supplement the previous, qualitativelybased studies. This paper reports an application of the Revised Universal Soil Loss Equation (RUSLE) within ageographical information system in order to estimate soil loss on the island, and particularly for the high-erosionareas. Results show that total soil loss on the island is estimated at 298 259 t year1, with soil loss from high-erosion areassumming 84 780 t year1 (28% of total soil loss). If all of the high-erosion areas were afforested, their soil loss would bereduced to 10 264 t year1, i.e. a reduction of 88% for the high-erosion areas and a reduction of 25% for the island. Thisstudy thus calls for soil and water conservation programs directed to these erosion-prone areas before the land degradationand environmental damage they are causing become irreversible. The methodological approach used in this work toquantitatively estimate soil loss from erosion-prone areas can be adopted in other countries as the basis for a nationwideerosion assessment in order to better inform environmental policy needs for soil and water conservation.

    Additional keywords: erosion risk mapping, GIS, priority action areas.

    Received 4 July 2012, accepted 19 December 2012, published online 31 January 2013

    Introduction

    Soil erosion is an environmental problem that exacerbates on-siteland degradation, while at the same time being a source ofsediment and pollutants that adversely affect off-site aquaticecosystems (Lal 2001). Mauritius Island is potentially at riskto soil erosion because of its rugged topography, extensivesugarcane cultivation, and tropical climate. This makes theland particularly vulnerable to erosion. In addition, otherecosystems can be damaged due to erosion, namely, estuaries,marshes, sh habitats, sea grass, and coral reefs.

    Conservation measures are needed to reduce the effects ofsoil erosion, and successful conservation programs require theconcentration of resources on priority action areas. Soil-erosionrisk assessment at a regional scale is commonly used to identifysuch conservation areas (e.g. Vrieling et al. 2002). The rstpublished study to map the erosion risk across the whole islandwas conducted by Nigel and Rughooputh (2010b), developing asoil-erosion risk-mapping model termed MauSERM (MauritiusSoil Erosion Risk Mapping). Four erosion factors, namelyrainfall, land cover, topography, and soil, were consideredduring the erosion risk mapping using the MauSERM model.Investigations were also made on the best way to combine the

    factors, and the decision rule methodology was chosen, as it canbe easily manipulated to mimic the complex interactions of allfour factors (as opposed to factorial scoring).

    A second study was later conducted by running the modelwith new datasets, where slope gradient was replaced with slopelength (inclusive of land parcels and drainage structure effects).The results illustrate that erosion sites occur commonly incultivated areas with steep slopes and erosion has a summer-dominant pattern caused by intensive summer rainfall (Nigel andRughooputh 2010a). This study was qualitatively based andenabled identication of priority action areas. Now, a morequantitative study is needed, as this can provide assistance inriver basin management and to indicate the order of magnitudeof soil erosion and sediment yield (de Vente and Poesen 2005).

    The aim of the present study is to compute soil loss estimatesfor Mauritius Island and especially for the priority action areas.The specic objectives are: (1) apply the Revised UniversalSoil Loss Equation (RUSLE) model for the whole island,(2) compute soil loss estimates for the high-erosion areas(HEA) initially mapped, and (3) dene a second approach formapping of HEA and derive estimates of RUSLE soil loss forthese HEA. In this second approach, the HEA can be mapped

    Journal compilation CSIRO 2012 www.publish.csiro.au/journals/sr

    CSIRO PUBLISHINGSoil Research, 2012, 50, 645651http://dx.doi.org/10.1071/SR12175

  • from only two factors such as land cover and slope gradient,which are readily available, instead of soil erodibility and lengthof slope, which are generally more difcult to map at large scaleas they require more geographical information system (GIS)datasets (see e.g. Vrieling 2006). The RUSLE soil map producedwill be the rst for Mauritius and will enable regional erosionevaluation for the determination of areas where soil conservationshould be emphasised.

    Materials and methods

    Study area

    Mauritius is in the south-west of the Indian Ocean (Fig. 1) atlatitude 208100S and longitude 578300E. The island has anelliptical shape with a major axis 63 km, minor axis 43 km,surface area 1859 km2, and highest peak 828m altitude. Theisland is of volcanic origin with eruptions lasting from 10 to0.025million years Before Present. Two main soil groups exist:mature Latosols originating from highly weathered, basaltic lava

    rock; and immature Latosolic soils with minerals still in theprocess of weathering. Most soils have high clay contents andhigh percentages of stone and organic matter content (organicmatter 311%). Soil depth is mainly 50100 cm, similar tomaximum plant rooting depth (Parish and Feillaf 1965).

    The climate is tropical maritime with two seasons: a rainysummer from November to April dominated by cyclonepassage, and a dry winter from May to October dominated bythe South-East Trade Wind and frontal systems. About 70% ofmean annual rainfall is received during summer. February is thewettest and hottest month, whereas October is the driest month.Mean annual rainfall is ~2000mm, equivalent to ~3700Mm3, ofwhich annual evaporation is 30%, surface runoff 60%, andgroundwater recharge 10% (WRU 2007). Surface runoff isconned within 213 river basins, which occupy 83% of theisland (Fig. 1) (Nigel and Rughooputh 2010a). Torrential owswith severe bank erosion and turbidity in the lagoon are commonduring intense rainfall events (Arlidge and Wong You Cheong1975).

    Fig. 1. Study area, Mauritius Island.

    646 Soil Research R. Nigel and S. D. D. V. Rughooputh

  • There is extensive sugarcane cultivation, which occupies54.1% of the island, while forest covers 26.7%, sparsevegetation 7.1%, urban areas 5.5%, scrub 2.9%, tea 1.6%,water bodies 0.9%, barren lands 0.5%, wetlands 0.4%,vegetables 0.2%, and sand 0.1% (Nigel and Rughooputh2010b). Sugarcane is harvested each year from July toOctober, during which the cane ratoon is not removed butleft over for regrowth and replaced usually every 57 years,at which time the whole eld undergoes tillage. Seeruttunet al. (2007) measured soil loss for ve sites for fourconsecutive years, with each site having two plots: one bareand the other planted with sugarcane. The rate of soil loss frombare plots was in the range 0.537.6 t ha1 year1, whilesugarcane reduced soil loss by 8099%. However, thesestudies were conducted only on plots having linear slopesand isolated from upslope contributing areas (soil type andrainfall erosivity did not vary over each plot size).

    Estimating soil loss pattern with RUSLE

    Like most qualitative models, one of the limitations ofMauSERM is that it provides qualitative outputs, which arenot linked to quantitative estimates of soil loss. These wouldhave been very useful for planning purposes, particularly for thehigh erosion areas. Converting erosion risk classes into estimatesof soil loss may be done by upscaling erosion measurementsfor selected sites, as proposed by Vrieling et al. (2002). In thepresent case, no erosion measurements for selected sites wereavailable to perform such an upscaling.

    Another approach would be the use of a quantitative erosionmodel, such as the RUSLE model (Renard et al. 1997) or its rstversion, the USLE (Wischmeier and Smith 1978). These modelsare widely used for modelling soil loss quantitatively, includingfor large areas by using a GIS (e.g. Lu et al. 2003). It must benoted that the original USLE model is a quantitative model, butapplication of the model at a regional scale within a GIS requiressimplication of the model, and therefore, its use within a GISis commonly referred to as a semi-quantitative modelling oferosion. The soil loss equation for the RUSLE model is given asfollows:

    A R K LS C P 1where A is the spatial average soil loss (t ha1 year1), R is therainfall erosivity factor (MJ.mmha1 h1 year1), K is the soilerodibility factor (t.hMJ1mm1), LS is the slope length andsteepness factors (unitless), C is the cover management factor(unitless, values ranging from 0 to 1), and P is the supportpractice factor (unitless, values ranging from 0 to 1).

    In the present case, we computed rainfall erosivity R usingEqn 2 (Arnoldus 1980), and which was found appropriate for uselocally (Le Roux et al. 2005):

    R 0:0302MFI1:9 2where MFI is the Modied Fournier Index, and is given byEqn 3:

    MFI Xi12

    i1

    Mi2A

    3

    where Mi is the rainfall amount received in month i and A is theannual rainfall amount.

    Values of soil erodibility for soil types (Table 1) wereobtained from Le Roux (2005) and Seeruttun and Ah Koon(2006). A map of slope length, LS, was obtained from Nigel andRughooputh (2010a), computed by taking into account landparcel effects along with the methodology of Desmet and Govers(1996) as specically implemented in the USLE2D software ofVan Oost and Govers (2000).

    Further data needed for running the RUSLE model above(Eqn 1) are the C and P values for land cover types. These C andP values are given in Table 2, which were obtained mainly fromLe Roux (2005), except for sparse vegetation (which has beenset the same as for forest). These values of C and P were thenassigned to a 10-m cell-size land cover map, resulting in tworaster maps (of C and P) suitable for raster processing of Eqn 1to produce a soil loss map. The land cover map was producedmainly from published map series (updated year 2005) (Nigeland Rughooputh (2010a).

    A second approach to identify high-erosion risk areas

    Another approach that can be used to establish the high-erosionareas of the island is the use of only two factors that can bedirectly mapped. A land cover map is one such factor. The otheris a slope gradient map, which requires less processing andfewer datasets compared with a land cultivation suitabilitymap, which in addition to topography requires information onsoil type. Initially, a land cultivation suitability map was used in

    Table 2. RUSLE C and P values for the different land cover types

    Land cover type C P

    Sugarcane 0.011 0.975Sparse vegetation 0.001 1.000Scrub 0.001 1.000Barren lands 0.011 1.000Tea 0.003 1.000Vegetables 0.204 0.625Forest 0.001 1.000Urban areas, water bodies, wetlands and sand Nil 1.000

    Table 1. RUSLE K soil erodibility values

    Soil order Soil type RUSLE erodibility K(t.hMJ1mm1)

    Zonal Low Humic Latosols, L 0.10Humic Latosols, H 0.10Humic Ferruginous Latosols, F 0.15

    Intrazonal Latosolic Red Prairie Soils, P 0.20Latosolic Brown Forest Soils, B 0.20Dark Mag Clay, M 0.10Grey Hydromorphic Soils, D 0.10Low Humic Gleys, G 0.20Ground Water Laterite, W 0.30Mountain Slope Complexes, S 0.15

    Azonal Lithosols, T 0.30Alluvial Soils, A 0.15Regosols, C 0.05

    RUSLE-based soil erosion modelling Soil Research 647

  • Nigel and Rughooputh (2010a), and it required (i) slopegradient, (ii) length of slope, (iii) soil erodibility, and (iv) apre-existing land suitability classication scheme [the onedened for Mauritius by Arlidge and Wong You Cheong(1975) was used]. Additionally, land cultivation suitabilitywould be more difcult to directly visualise in the eldcompared with steep slope gradients alone.

    As such, based on land cover and slope gradient, a morestraightforward denition of HEA can be obtained. Thisalternative HEA will henceforth be termed HEA-B. Inessence, HEA-B can be mapped based on the occurrences ofcrop cultivation on slopes >20%. In a GIS, this is achieved byextracting land cover classes that show cultivation (sugarcane,tea, and vegetables) and intersecting this dataset with a slopegradient map that shows only values >20%.

    Results and discussion

    Here, results of the second approach are presented rst, followedby results of the RUSLE modelling. Results of the mapping of

    HEA-B show that 58 km2 of land has slopes >20% and is beingcultivated (with sugarcane 98.8%, vegetables 0.06%, and tea1.14%). The extent of HEA-B is thus about four times less thanthat of the original HEA (58 v. 251 km2).

    The spatial distribution of the established HEA (originalHEA and HEA-B) is shown in Fig. 2. In the event that notall of the 251 km2 of the original HEA will be the focus forconservation efforts (due to nancial constraints, for instance),then at least the areas dened as HEA-B, and particularly thesugarcane elds, must be targeted for conservation efforts.

    The map of soil loss produced using the RUSLE model isshown in Fig. 3. The soil loss estimates were classied usingthe scheme of Le Roux et al. (2005) for Mauritius. The highestsoil-loss values are mostly distributed within the steep,cultivated hilly areas. The total soil loss on the island isestimated at 298 259 t year1. Accordingly, based on RUSLErelative modelling, concerning the alternative denition ofhigh-erosion areas (HEA-B), it is seen that total soil lossfrom the sugarcane elds of HEA-B is 63 673 t year1, which

    High Erosion Areas

    HEA-B

    HEA

    N

    0 5 10

    km

    Fig. 2. High erosion areas of Mauritius Island: HEA and HEA-B.

    648 Soil Research R. Nigel and S. D. D. V. Rughooputh

  • is 66% of total soil loss from all sugarcane elds on the island.Thus, while sugarcane on steep slopes occupies only 58 km2 ofthe 1006 km2 of land cultivated with sugarcane, it is nonethelesscontributing to 66% of total soil loss from all sugarcane eldsand contributing to 21% of overall soil loss on the island. If atleast these sugarcane elds of HEA-B were afforested, their totalsoil loss would be reduced to 7641 t year1, which would reducesoil loss from all sugarcane elds by 58% and reduce overall soilloss by 19% (Table 3).

    Nonetheless, the rst proposal for conservati...

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