7 research outputs found
Soil related constraints for sustainable intensification of cereal-based systems in semi-arid central Tanzania
Effectiveness of phosphate rock on ferralsols in Tanzania and the influence of within-field variability
Crop yields in Tanzania are often limited by P deficiency. Direct application of the locally mined Minjingu phosphate rock (MPR) is considered a possible option in addressing the problem. Being poorly soluble, it is more effective in low pH soils with sizeable P and Ca sinks. In soils rather high in pH, mechanisms are required to promote its dissolution. This research was initiated with the overall objective of increasing our understanding of the multiple interactions affecting the availability of P from MPR in the soil-plant system. This knowledge is required to enable optimal exploitation of the various factors influencing MPR effectiveness for increased crop production. The research program consisted of one laboratory experiment, six greenhouse experiments and four field trials.The laboratory and greenhouse experiments dealt with single factors influencing the effectiveness of PR under controlled conditions. From the laboratory experiment it was established that the high content of CaCO 3 in Minjingu PR was the major factor that determined the amount of HCl extractable P. However, agronomically it did not differ from Khouribga and Mali PRs, which have relatively lower CaCO 3 content. High application rates lowered the effectiveness of PR pointing to a need to balance application rates with proton supply. In a study relating yield and soil pH, increasing dry-matter yield of maize, cowpea and pigeonpea could not noticeably affect the soil pH mainly due to the pH buffer capacity of the soils. However, when intercropped with maize, cowpea or pigeonpea took up more P from MPR and even improved the uptake of MPR-P by maize. This point to a possible proton induced dissolution of MPR by the legumes. Hence, when intercropping involves legume crops capable of fixing N lower rates of PR can be used which is an attractive option for resource poor farmers. A study on the response of maize, cowpea and pigeonpea to MPR and TSP on soils of low and high pH showed that response to MPR was stronger in the low than in the high pH soil. Both legumes gave a higher DM production with MPR than with TSP on the high pH soil and yields were higher on the high than on the low pH soil. This indicates that the legumes prefer a high soil pH to a low soil pH and are able to make use of MPR at a relatively high pH. The later is possible when the legumes can modify rhizosphere soil conditions with respect to pH.Maize dry-matter yield response to P on soils with different pH and available P was observed where soil available P was low. There was no yield response to P when P-Bray-I was > 7 mg kg -1 (P-Olsen > 10 mg kg -1 ). Utilization of absorbed P was better from MPR than from TSP in low pH soils indicating a liming effect by the MPR.Field experiments dealt with multiple factors influencing the effectiveness of PR. The influence of spatial soil variability on the effectiveness of PR and crop performance was studied using the Post-mortem Residual Analysis and Nearest Neighbor Means techniques. These techniques were effective in isolating environmental from treatment effects and they were more useful in the large than in the small trials. A study on the method and rate of P application showed that method of application was more important for MPR in high pH soils and that response to MPR will be obtained at modest rates. The residual effects of TSP and MPR were almost the same. Combined application of MPR and the acidifying fertilizer sulfate of ammonia showed that there is little scope for improving the effectiveness of MPR through the acidifying effect of sulfate of ammonia. Combined application of MPR and TSP gave best results in low pH soils when both of them were applied using the same method. Meanwhile, incubating MPR with farmyard manure could not stimulate MPR dissolution given the high pH of the two materials even after 40 days of incubation (pH (H 2 O) = 8.35). It is concluded that the use of MPR could be extended to less acidic P deficient soils when mechanisms are employed that could stimulate its dissolution. They include use of low amounts of MPR (low input strategy), incorporating legumes in the cropping system and using the same method of application of mixtures of MPR and soluble P fertilizers.Keywords: Minjingu phosphate rock, triple superphosphate, Rhodic Ferralsols, farmyard-manure, protons, dissolution, legumes, maize, management options, spatial soil variability, Tanzania.</p
Using local resources to improve soil fertility in Tanzania
SIGLEAvailable from British Library Document Supply Centre-DSC:5359.2826(no 21) / BLDSC - British Library Document Supply CentreGBUnited Kingdo
RPE PLaW
The paper documents experiences of Lushoto farmers' innovations on introduced technologies. It discusses methodology, farmer innovations so far, the benefits that farmers think they are gaining, mechanisms for sharing innovations, and the issues that arise and possible impact on the scaling out process from farm level to watershed level. Farmers seemed to innovate on introduced technologies to adapt and fit them into their farming systems, financial status, age and social circumstances, and whether they need collective action to implement innovations. However, the challenge remains: will the modified technologies spill over to more farmers
The importance of proton supply in phosphate rock dissolution: Comparative study of three phosphate rocks from sub-Saharan Africa
The dissolution in hydrochloric acid of three phosphate rocks (PRs) from sub-Saharan Africa was studied in the laboratory and their agronomic effectiveness compared using soils from Tanzania, Ivory Coast, Kenya and Netherlands. The objective was to investigate the potential of the PRs in supplying phosphorus under conditions of limited and unlimited supply of protons (H+). The test crop was maize (Zea mais var. LG11). Results show that calcium carbonate content is an important factor determining differences between the PRs with respect to their effectiveness. They also show that (i) differences in the dissolution of the PRs manifested more at low than at high acid concentration, (ii) availability of enough protons is an important factor in PR dissolution, (iii) low rates of PRs should be more desirable than high rates and (iv) soil and plant factors have an important role in the effectiveness of a PR
Soil fertility evaluation and management by smallholder farmer communities in northern Tanzania
The objective of this paper is to compare soil fertility evaluation based on experience and knowledge of smallholder farmer communities with the evaluation by scientists based on soil analysis and model calculations. The role of the smallholder farmer community in soil fertility evaluation and management was examined from two `research for development¿ projects in northern Tanzania. These are the African Highlands Initiative (AHI) and the Soil Water Management Research Group (SWMRG). Participatory approaches were applied by both projects. Farmers¿ experience and knowledge of local indicators of soil quality were used in identifying soil fertility constraints and in generating resource flow maps. The farmers¿ evaluation of soil fertility was compared with soil analytical data and with calculations of maize yields by the model QUEFTS. Farmers¿ indigenous knowledge in soil fertility evaluation mostly agreed with laboratory analysis and model calculations by QUEFTS. Model calculations identified potassium as the most limiting nutrient in the highlands in northeastern Tanzania for yields less than 3 t ha¿1 and phosphorus for yields higher than 4 t ha¿1. In Maswa (Lake Victoria Basin) nitrogen was most limiting. Given that farmers¿ evaluation of soil fertility is relative to what they see around them, there is a need to verify their observations, but also the interpretation of laboratory data by models like QUEFTS requires continuous and critical validation. Both projects have shown that there is scope to reverse the trends of declining soil fertility in smallholder farms in northern Tanzania. Essential was that the interaction with scientists has built confidence in the farmers because their knowledge in addressing soil fertility constraints was recognized