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Applied and Environmental Soil Science
Volume 2013 (2013), Article ID 601058, 7 pages
A Case of Cyperus spp. and Imperata cylindrica Occurrences on Acrisol of the Dahomey Gap in South Benin as Affected by Soil Characteristics: A Strategy for Soil and Weed Management
1Felix Houphouet Boigny University, Soil Science Department, 22 BP 582, Cocody, Abidjan 22, Cote d'Ivoire
2University of Abomey-Calavi, Departement of Agronomy Sciences, BP 499, Calavi, Benin
3Africa Rice Center, BP 2031, Cotonou, Benin
4CIRAD, UPR Hortsys, 34398 Montpellier Cedex 05, France
Received 7 October 2012; Revised 15 April 2013; Accepted 28 April 2013
Academic Editor: Philip J. White
Copyright © 2013 Brahima Kone et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Because of the limiting efficacy of common weed control methods on Cyperus spp. and Imperata cylindrica their occurrences in tropical agroecologies and the effect of soil properties in suppressing these species were investigated in south Benin (Cotonou), a typical ecology of the Dahomey gap. Weeds and soil samples were collected twice early and later in the rainy season in 2009 at four topographic positions (summit, upper slope, middle slope, and foot slope). Sampling was done according to Braun-Blanquet abundance indices (3 and 5) and the absence (0) of Cyperus and Imperata in a quadrat, respectively. The relationship between their respective abundances and soil parameters (texture, C, N, P, K, Na, Ca, Mg, and Fe) was explored. Weed occurrence was less related to soil texture, and Imperata growth was more influenced by soil nutrients (K, Ca, and Fe) than Cyperus spp. Soil cation ratios of K : Mg and Ca : Mg were the main factors that could be changed by applying K and/or Mg fertilizers to reduce Cyperus and/or Imperata occurrence. Maintaining high Fe concentration in soil at hillside positions can also reduce Imperata abundance, especially in the Dahomey gap.
Weeds are notorious yield reducers that are, in many situations, economically more important than insects, fungi, or other pest organisms [1, 2]. The yield loss due to weeds is almost always caused by an assemblage of different weed species, and these can differ substantially in competitive ability . In rice growing agro-ecologies of West Africa, weed species assemblages include nutsedges and speargrass that are perennial and serious threats .
Imperata cylindrica (L.) Raeuschel (speargrass) is a common and persistent weed in upland ecology. It reproduces through seeds and rhizomes. This weed is particularly difficult to control, as it is tolerant to fires and shallow cultivation due to its extensive underground network of rhizomes. The weed tends to be abundant where fields are regularly cultivated and burnt, as it recovers rapidly from disturbance, and burning induces flowering. It exerts great competition on crops [5, 6].
In moist to hydromorphic upland areas, some of the most intractable weed problems in rice are due to the perennial sedges Cyperus rotundus L. (purple nutsedge) and Cyperus esculentus L. (yellow nutsedge). Their tubers and seeds can remain dormant to survive periodic flooding or dry seasons. These species are able to multiply rapidly through tubers which can be greatly accelerated by soil tillage . Because of these characters, I. cylindrica and Cyperus spp. are typical weeds of intensively cultivated lands and very difficult to control .
Some relative successes were observed using chemical methods for the control of Cyperus spp. and I. cylindrica . But, herbicide is expensive and not always available to West African smallholder farmers. Moreover, there is a risk of environmental pollution. Therefore, additional knowledge and technology are needed for improving the control of Cyperus spp. and Imperata cylindrica in Africa, especially in the Dahomey gap (south Benin) where they are seriously threatening livelihoods .
Considering that reduced soil fertility often increases weed infestation  and the effects of soil parameters in weed occurrence in Nigeria , the concept of chemotropism  is hypothesized in order to identify soil nutrients (N, P, K, Ca, Mg, and Fe) that influence the occurrence of Cyperus spp. and /or Imperata cylindrical attention should be paid to topography and soil texture influencing soil organic matter that can change vegetation structure .
A nonsite replicated ecological study  was initiated during the rainy season of 2009 along a catena of Acrisol in south Benin (West Africa), which is a typical ecology of the Dahomey gap. The implication of soil texture and nutrients (C, N, P, K, Ca, Mg, and Fe) on the occurrence of Cyperus spp. and I. cylindrica in this upland agro-ecology was explored. The aim was to identify soil parameters that can be used to develop a management strategy for the control of these perennial weeds in continued rice growing agro-ecologies of the Dahomey gap.
2. Materials and Methods
2.1. Site Description
The study was conducted during the 2009 cropping period (June–September) at the Africa Rice Center (ex-WARDA) experimental station in Cotonou (6° 28 N; 2° 21 E, 15 m asl), Benin. The site is a derived savanna zone in the Dahomey gap of West Africa. The rainfall pattern was bimodal with 807 mm during the cropping season of 2009. The soil is locally named “terre de barre.” It is a very deep Acrisol (>10 m), with sandy top soil (0–40 cm) and free of constraints (gravels, stones, or hardpan) to plant rooting in the profile. Soil pHwater was 5 and C : N, Ca : Mg and K : Mg ratios were about 12, 1.7 : 1 and 1 : 1, respectively. The studied area is continuously cultivated for upland rice production.
2.2. Weed Sampling
Two dominance-abundance indices were considered for Cyperus spp. and Imperata cylindrica as a proportion of weeds in 1 m2 quadrats: 3 = covering between 1/4-1/2 of the soil surface and 5 = covering more than 3/4 of the soil surface . Weeds were also sampled where Cyperus and Imperata were absent, and zero (0) was the corresponding index. Indices 0, 3, and 5 were considered as absent (A), medium density (M), and high density (H), respectively. Three sampling places (A, M, and H) were identified for each of Cyperus spp. and I. cylindrica in the summit, the upper slope, the middle slope, and the foot slope as described by Ruhe and Walker . Sampling was replicated twice in the studied site: in July (1) and in September (2) at the beginning and the end of the rainy season, respectively. In a quadrat, all the weed species were sampled separately with bellow ground dry matter. Individual identification was done as described by Akobundu and Agyakwa  and they were coded according to Braun-Blanquet . The roots were cut off, and weeds were oven dried at 70°C for 24 hours before weighting.
2.3. Soil Sampling and Analysis
Topsoil (0–20 cm depth) was sampled using augur (20 cm × 7 cm) in each quadrat at every time of weed sampling. After sampling weeds, a soil sample was taken from the centre of the quadrat. Twenty-four (24) soil samples (12 at each sampling time) were taken, and sun dried before laboratory analysis. Soil particle sizes were determined by the Robinson pipette method  as well as organic-C, total-N, P-available (BrayI), and total-P (Pt). Soil exchangeable K, Ca, Mg, and extractable Fe were also determined. Chemical analyses were performed as described by Page et al. .
2.4. Statistical Analysis
Descriptive statistics were used to calculate the frequency of weed species in a specific quadrat. By analysis of variance (ANOVA), mean values of soil particle size and nutrients were determined for each topographic section. Mean values of total weed biomass dry matter were also determined for each placement of quadrat. The mean values were separated by Student-Newman and Keul methods. The relationships between biomass dry matter and soil physical and chemical characteristics were evaluated by Pearson correlation. SAS 10 package was used for these analyses. Soil clay, sand, C, N, Pa, K, Ca, Mg, and Fe concentrations were used to discriminate Imperata abundance indices (3 and 5) and absence (0) by canonical function analysis using SPSS 16.
3.1. Soil Characteristics
The topsoil (0–20 cm) was sandy, and the middle slope (MS) had a significantly greater proportion of sand than other positions (Table 1). This topographic position also had significant lower contents of clay (11%) and silts (4%). The soil had moderate carbon content throughout the toposequence except in the soil at foot slope (FS) position; where it was significantly higher, similar gradient was observed for total nitrogen-Nt content along the toposequence. Phosphorus (P-available and P-total) contents were moderate in the soils of upper slope (US) and MS while they were higher in the soils at summit (SUM) and FS positions. Soil concentrations of divalent cations (Ca and Mg) were significantly higher at the SUM position with a decreasing trend along the toposequence. Similar result was observed for soil Fe concentration. Meanwhile, monovalent cations (K and Na) concentrations contrasting with these results with an increasing trend from the SUM to the FS.
3.2. Weed Assemblages
Seventeen weed species were most frequently encountered in the quadrats. Other species were also observed in at very low frequencies, and their cumulative frequencies were depressed in the medium and high densities of Cyperus spp. and I. cylindrical, respectively (Figure 1). However, more diverse communities were observed where Cyperus spp. and I. cylindrica were recorded in the quadrats compared to places where they were absent. Nevertheless, Richardia brasiliensis (Ricbr) was encountered in all quadrats with moderate (9.09%) to high (21.74%) frequency and Dactyloctenium aegyptium (Dacae) at a low frequency (2.56%–8.82%), about 14% in 1 m2 characterized the medium density of Cyperus spp. and I. cylindrica occurrence, respectively. Three species of Cyperus including Cyperus esculentus, Cyperus sphacelatus, and Cyperus rotundus were identified. But only Cyperus rotundus (Cypro) was encountered for the medium density of Cyperus spp. Whenever high densities of Cyperus and Imperata were observed, they accounted for 25.92% and 20.51%, respectively. Commelina erecta (10.26%) and Richardia brasiliensis (12.82%) were the most frequent weed species associated with the high density of Imperata.
Figure 2 shows the mean values of total weed biomass dry matter for each quadrat according to Imperata and Cyperus densities. Weed biomass was significantly higher in quadrats with high densities for Imperata and Cyperus, respectively. Wherever Cyperus and Imperata were absent, total weed biomass did not differ significantly with that observed for their medium densities.
3.3. Weed and Soil Relations
Table 2 shows the Pearson correlation values (R) between soil characteristics and the biomass of Cyperus and Imperata, respectively, when high densities were observed. Carbon-C (−0.34), N (−0.39), Pa (0.55), and Ca (−0.36) had highest correlation values with Cyperus biomass, but these results were not significant. Meanwhile, highly significant () correlations were observed between the biomass of Imperata and K (0.73), Ca (−0.84), and Fe (−0.88) concentrations in the soil. Moreover, clay (−0.66) and silt (0.62) had significant correlation with Imperata biomass at certain level of probability ().
Figure 3 shows that group centroids (mean of the discriminant score for a given category of dependant variable) of Imperata abundance indices are well separated, attesting the ability of soil parameters (clay, sand, Pa, C, N, K, Ca, Mg, and Fe) to discriminate Imperata density: absence was mainly characterized by lower Fe and Pa concentrations in soil, while increasing of soil sand, clay, Pa, and Mg was characterized by abundance (5). The medium (3) density of Imperata was observed for low soil C and Ca contents.
Table 3 shows variance of these relationships according to topographic positions. In fact, the highest soil clay (14%), Fe (3509.5 ppm), and K (0.04 cmol kg−1) concentrations were associated with the abundance of Imperata at the summit. However, the absence of Imperata at the US and MS positions was more related to high soil Fe concentration. Highest (US) and lowest (MS) K concentration in soil characterized the highest density and the absence of Imperata, respectively, according to topographic positions. Soil calcium concentrations were not significantly different for the absence and the high density of Imperata at the SUM and the US. In contrast, the highest (2.44 cmol kg−1) and lowest (2.00 cmol kg−1) soil Ca concentrations were related to high density of Imperata at the FS and MS positions, respectively.
4.1. Extension and Limit of Our Finding
Cyperus esculentus, Cyperus sphacelatus, and Cyperus rotundus were encountered in the studied area. The last species was the most frequent along the toposequence compared to the others. However, the occurrence of Cyperus sphacelatus contrasts with observations by Johnson  who mentioned the occurrence of Cyperus difformis in rice agro-ecosystems rather than C. sphacelatus. Dactyloctenium aegyptium (Dacae), Richardia brasiliensis (Ricbr), and Commelina erecta (Comer) were the most frequent weed species associated with Cyperus and Imperata according to our study which differs from previous knowledge of weed community in upland ecology of West Africa . Furthermore, Andropogon, Cymbopogon, Hyparrhenia, Pennisetum, and Setaria were frequently encountered in the southern guinea savanna including Brachiaria spp. instead of Setaria identified in the northern guinea savanna of West Africa . Therefore, the studied location in the Dahomey gap differs from the ecologies of north and south guinea savanna of West Africa. Indeed, the studied zone was described as a costal savanna  representing a marginal zone of West Africa, which was named the Dahomey gap . Therefore, this particularity could have induced differences in weed assemblages compared to the others savanna ecologies. Hence, our analyses provide additional knowledge of weed occurrence in rice growing agro-ecologies of West Africa.
The studied ecology was also characterized by a landscape of a wide plateau with depressions instead of a hydrographic network as described by Raunet  on the crystalline basement of West Africa. However, the trends of variation in soil nutrients were the same along the toposequence of terre de barre as described elsewhere : divalent cations concentrations decreased from the summit to the foot slope, while soil concentrations of monovalent cations increased. Therefore, the influence of soil parameters on weed species occurrence as revealed in our actual study can be considered for the entire Dahomey gap and the other ecologies of West Africa according to the rule of nonreplicated ecological study .
4.2. Weeds Control by Soil Fertility Management
The lowest total weed biomass was observed in the quadrats when Cyperus and Imperata were absent. This result attested that factors affecting the occurrence of these species can also be considered for the others weeds species. Therefore, our result provides an insight to deeper knowledge of the interactions of divers weed communities with soil. However, exceptions should be considered for Richardia brasiliensis (Ricbr) and Dactyloctenium aegyptium (Dacae) which were encountered in all the quadrats (Figure 1) indifferently to the density of Cyperus and Imperata.
No significant relationship was observed between the soil parameters studied and Cyperus spp. biomass (Table 2). However, Koné et al.  showed a decreased of Cyperus abundance with the increasing soil Mg concentration. Indeed, our study revealed some implications of this nutrient (Mg) in Cyperus occurrence through the soil balance of K and Mg, excepted in the FS position (Table 4). Application of K fertilizer might be able to increase soil K : Mg ratio and decrease Cyperus abundance at the SUM, while supplying Mg might induce the same effect on Cyperus occurrence at the US and MS positions by altering the Ca : Mg ratio. Therefore, K or Mg amendments are required for depressing Cyperus occurrence according to topographic positions. Indeed, soil balance in K : Mg and Ca : Mg can affect not only K and Ca availability to plant but also P as observed by Yates . Thus, it appears that Cyperus occurrence is more related to imbalanced ratio of nutrients in soil rather than the depletion effect of sole nutrient content.
I. cylindrica occurrence was significantly influenced by soil Fe, Ca and K concentrations with less importance to soil particle sizes (Table 2). This result restricts the assertion made by Andreasen and Streibig  concerning the influence of soil texture on weed occurrence. Furthermore, the influence of soil nutrients was confirmed partially according to topographic positions. Highest soil K concentration was associated with high density of Imperata at the uphill position (SUM and US). Instead of reducing soil K concentration for depressing the density of Imperata, management strategy must focus on reduction of K : Mg by supplying Mg compound as consequence of Pearson correlation value observed in Table 4. Imperata density can also decrease at the downhill position with the decrease or increase of soil Ca concentration at the MS and the foot slope positions, respectively. However, no consistent management of soil Ca can be drawn from our study regarding the contrasts observed in Tables 3 and 4. Further investigations should also focus on K : Ca: Mg or [() : K] ratio for improving knowledge of the interaction between Ca and Imperata. Up to now, our study has improved knowledge of the effect of soil nutrients balance on weed occurrence as mentioned by the Midwest Organic and stainable Education Service (MOSES) .
4.3. Indicators of Soil Degradation in the Environment
The study revealed that highest soil Fe concentrations at the Hillside (US and MS) were also associated with a low density of Imperata. Otherwise, Fe leaching as observed in degraded soil  may be favorable to Imperata occurrence depending on topographic positions. Low soil K (0.03–0.08 cmol kg−1) concentrations observed at the US position reinforced (Table 3) this assertion. Indeed, low K concentrations in soils of Africa occur generally in degraded soils according to Juo and Grimme . Therefore, our finding confirms the fact that Imperata is a bioindicator of degraded soil as propounded by Scherr and Yadav .
The leaching of soil K and Mg leads to impoverishment of soil in these nutrients, justifying their requirement for the control of Cyperus spp. occurrence, especially by changing soil nutrient balance. Thus, soil chemical degradation can also induce Cyperus spp. occurrence and likewise for Imperata. In the Philippines, Imperata cylindrica and Cyperus compressus were observed in strongly weathered soil  corroborating our analysis and suggesting that soil organic amendment can reduce the invasion of these species, especially for Cyperus . In the context of land management, we can recommend further study of fallowing or the cultivation of cover crops on Cyperus spp. and Imperata occurrences on Acrisols. These practices might be able to avoid soil degradation , restricting Cyperus and Imperata invasions.
Most of the knowledge of upland soil chemical degradation processes is related to nutrient depletion [35, 36]. Nutrient ratios have been investigated less frequently. Except for soil C (1.09–1.71%) and N (0.05–0.08%) concentrations and K (0.1 cmol kg−1) concentrations at certain levels of significance, the studied soil had high nutrient concentrations, especially for P (8–26.4 ppm) and Na that reached 0.55 cmol kg−1 (Table 1). But rice yield can drop to 0.26 tha−1 even for improved varieties with a potential yield of 4-5 tha−1, as a consequence of mineral imbalances, particularly C : N, Ca : Mg and K : Mg . Regarding yield reduction as an indicator of agricultural soil degradation , we deduce that unbalanced soil nutrients in the studied area are likely to contribute. These characteristics (nutrient ratios) of soil were also involved in rice P-nutrition in an acid Ferralsol of Nigeria . More investigations for understanding the effects of nutrient ratios in soils are required in tropical ecologies for improvement of agricultural land use, weed management, and restoration of degraded soils.
Our results showed association of high density of Imperata to Commelina erecta and Richardia brasiliensis. Finally, Imperata, Cyperus, Commelina, and Richardia can be considered as indicators of degraded Acrisols in the studied environment. The importance of soil exchangeable cation concentrations (Ca, Mg, Fe, and K) and the ratios of Ca : Mg and K : Mg for weeds occurrence in the Dahomey gap, and West African ecosystems by extension, confirms the work done by Udoh et al.  citing the importance of soil C, N, Zn, and Mn contents.
Soil parameters have influence the occurrence of weeds according to topographic positions, especially for Cyperus spp. and Imperata Cylindrica. However, the relationship with Cyperus spp. was less pronounced than with Imperata Cylindrica.
Soil balance, and in particular K : Mg and Ca : Mg ratios, were the main factors affecting the occurrence of these weeds in the studied ecosystem. Applying Mg and/or K fertilizers might be employed to change these soil characteristics to reduce Imperata and Cyperus invasions. Soil Fe concentration also influenced Imperata occurrence. It is suggested that Cyperus and Imperata occurrences prevailed in degraded soil for which they can be used as indicators, along with Commelina and Richardia. To some extent, our finding can be extended to other West African ecosystems.
- S. Savary, R. K. Srivastava, H. M. Singh, and F. A. Elazegui, “A characterisation of rice pests and quantification of yield losses in the rice-wheat system of India,” Crop Protection, vol. 16, no. 4, pp. 387–398, 1997.
- S. Savary, L. Willocquet, F. A. Elazegui, N. P. Castilla, and P. S. Teng, “Rice pest constraints in tropical Asia: quantification of yield losses due to rice pests in a range of production situations,” Plant Disease, vol. 84, no. 3, pp. 357–369, 2000.
- S. E. Weaver and J. A. Ivany, “Economic thresholds for wild radish, wild oat, hemp-nettle and corn spurry in spring barley,” Canadian Journal of Plant Science, vol. 78, no. 2, pp. 357–361, 1998.
- D. E. Johnson and R. J. Kent, “The impact of cropping on weed species composition in rice after fallow across a hydrological gradient in west Africa,” Weed Research, vol. 42, no. 2, pp. 89–99, 2002.
- D. E. Johnson, Weeds of Rice in West Africa, WARDA, Bouaké, Côte d'Ivoire, 1997.
- D. Chikoye, V. M. Manyong, and F. Ekeleme, “Characteristics of speargrass (Imperata cylindrica) dominated fields in West Africa: crops, soil properties, farmer perceptions and management strategies,” Crop Protection, vol. 19, no. 7, pp. 481–487, 2000.
- L. G. Holm, D. L. Plucknett, P. V. Pancho, and J. P. Herberger, The World’s Worst Weeds: Distribution and Biology, University Press of Hawaii, Honolulu, Hawaii, USA, 1991.
- J. Rodenburg and D. E. Johnson, “Chapter 4—weed management in rice-based cropping systems in Africa,” Advances in Agronomy, vol. 103, pp. 149–218, 2009.
- J. Townson, “Imperata cylindrica and its control,” Weed Abstracts, vol. 40, pp. 457–468, 1991.
- P. V. Vissoh, Participatory development of weed management technologies in Benin [Ph.D. thesis], Wageningen University, Wageningen, The Netherlands, 2006.
- H. R. Mohammaddoust, A. M. Tulikov, and M. A. Baghestani, “Effect of Long-term fertilizer application and crop rotation on the infestation of fields by weed,” Pakistan Journal of Weed Science Research, vol. 12, no. 3, pp. 221–234, 2006.
- B. T. Udoh, A. O. Ogunkunle, and N. U. Ndaeyo, “Influence of soil series and physic-chemical properties weed flora distribution at Moor plantation Ibadan, Southern Nigeria,” Journal of Agriculture & Social Sciences, vol. 3, no. 2, pp. 55–58, 2007.
- J. C. Nekola, “Vascular plant compositional gradients within and between Iowa fens,” Journal of Vegetation Science, vol. 15, no. 6, pp. 771–780, 2004.
- P. B. Hook and I. C. Burke, “Biogeochemistry in a shortgrass landscape: control by topography, soil texture, and microclimate,” Ecology, vol. 81, no. 10, pp. 2686–2703, 2000.
- K. H. Reckhow, “Bayesian inference in non-replicated ecological studies,” Ecology, vol. 7, no. 6, pp. 2053–2059, 1990.
- J. Braun-Blanquet, Pflanzensoziologie. Grundzüge DerVegetationskunde, vol. 7, Biologische Studienbücher, Berlin, Germany, 1928.
- R. V. Ruhe and P. H. Walker, “Hillslope models and soil formation:I. Open systems,” in Proceedings of the Transactions of the 9th International Congress on Soil Science, vol. 4, pp. 551–560, 1968.
- I. O. Akobudu and C. W. Agyakwa, Guide to West African Weeds, IITA, Ibadan, Nigeria, 1987.
- G. W. Gee and J. W. Bauder, “Particle-size analysis,” in Methods of Soil Analysis. Part 1. Physical and Mineralogical Methods, A. Klute, Ed., vol. 9 of Agronomy, Madison, Wis, USA, 2nd edition, 1986.
- A. L. Page, R. H. Miller, and D. R. Keeney, Methods of Soil Analysis, Chemical and Microbiological Properties. Part 2, vol. 9 of ASA Monograph, American Society of Agronomy, Madison, Wis, USA, 2nd edition, 1996.
- P. N. Windmeijer and W. Andriesse, “Inland Valleys in West Africa: An Agro-Ecological Characterization of Rice-Growing Environments,” International Institute for land Reclamation and Improvement. Pub. 52. Wageningen, The Netherlands, 1993.
- B. Koné, G. L. Amadji, M. Igué, and O. Ayoni, “Rainfed upland rice production on a derived savannah soil of West Africa,” Jounal of Animal and Plant Science, vol. 2, no. 4, pp. 156–162, 2009.
- B. Koné, G. L. Amadji, S. Aliou, S. Diatta, and C. Akakpo, “Nutrient constraint and yield potential of rice on upland soil in the South of Dahomey gap of West Africa,” Archieve of Agronomy and Soil Science, vol. 57, no. 7, pp. 763–774, 2011.
- M. Raunet, “Les bas-fonds en Afrique et à Madagascar. Géomorphologie, géochimie, pédologie, hydrologie,” Zeitschrift Fuer Geomorphologie, vol. 52, pp. 25–62, 1985.
- B. Koné, S. Diatta, O. Sylvester et al., “Estimation de la fertilité potentielle des ferralsols par la couleur,” Canadian Journal of Soil Science, vol. 89, no. 3, pp. 331–342, 2009.
- B. Koné, A. Touré, G. L. Amadji, A. Yao-Kouamé, T. P. Angui, and J. Huat, “Soil characteristics and Cyperus spp. occurrence along a toposequence,” African Journal of Ecology, 2013.
- R. Yates, “Yield depression due to phosphate fertilizer in sugarcane,” Australian Journal of Agricultural Research, vol. 15, no. 4, pp. 537–547, 1964.
- C. Andreasen and J. C. Streibig, “Impact of soil factors on weeds in Danish cereals crops,” Weed Abstract, vol. 39, pp. 434–435, 1990.
- MOSES, “The importance of organic matter to soil fertility and crop health,” MOSES Organic Fact sheet, http://www.mosesorganic.org/MOSES%20fact%20sheet/22SeasonExtens, 2009.
- J. Roose, Dynamique actuelle d’un sol ferrallitique sablo-argileux très désaturé sous culture et sous foret dense humide sub-équatoriale du Sud de la Côte d’Ivoire, ORSTOM, Abidjan, Côte d'Ivoire, 1980.
- A. S. R. Juo and H. Grimme, “Potassium status of major soils in tropical Africa with special refrence to potassium availability,” in Proceeding of the Potassium Workshop Jointly Organized by IITA and the International Potassium Institute, IPI, Berne, Switzerland, October 1980.
- S. J. Scherr and S. Yadav, Land Degradation in the Developing World Implications for Food, Agriculture, and the Environment to 2020, International Food Policy Research Institute, Washington, DC, USA, 1996.
- I. A. Navarrete, V. B. Asio, R. Jahn, and K. Tsutsuki, “Characteristics and genesis of two strongly weathered soils in Samar, Philippines,” Australian Journal of Soil Research, vol. 45, no. 3, pp. 153–163, 2007.
- A. M. Whitbread, O. Jiri, and B. Maasdorp, “The effect of managing improved fallows of Mucuna pruriens on maize production and soil carbon and nitrogen dynamics in sub-humid Zimbabwe,” Nutrient Cycling in Agroecosystems, vol. 69, no. 1, pp. 59–71, 2004.
- L. R. Oldeman, “Global extent of soil degradation,” in Soil Resilience and Sustainable Use, L. R. Oldeman, Ed., pp. 99–118, CAB International, Wallingford, UK, 1994.
- G. W. J. Van Lynden and L. R. Oldeman, The Assessment of the Status of Human-Induced Soil Degradation in South and Southeast Asia, ISR IC, Wageningen, 1997.
- B. Koné, S. Diatta, A. Saidou, I. Akintayo, and B. Cissé, “Réponses des variétés interspécifiques du riz de plateau aux applications de phosphate en zone de forêt au Nigeria,” Canadian Journal of Soil Science, vol. 89, pp. 555–565, 2009.