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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Reuben, Salum Kihiri | - |
| dc.date.accessioned | 2026-05-25T06:03:16Z | - |
| dc.date.available | 2026-05-25T06:03:16Z | - |
| dc.date.issued | 2021-05 | - |
| dc.identifier.uri | http://localhost:8081/jspui/handle/123456789/21061 | - |
| dc.guide | Kasiviswanathan, K.S . | en_US |
| dc.description.abstract | Water Resources Management is a many-sided process that requires the entanglement of many other pieces of information to underpin various decisions in society. The land surface and water are the important resources of the universe, therefore, they have to be well maintained since they are ecologically sound. However, among the prerequisites for any proper planning for agriculture and Management of rivers are the details on erosion and sediments. Time and again, sediment distribution in rivers usually brings on dwindling of the storage area, the life cycle of reservoirs, the quality of water, river discharges leads to water shortage for other several usages, likewise, sediments induce uneconomical purification methods for water. Modeling may deliver a measurable and compactible technique to evaluate soil and sediment yield erosion based on a vast scope of circumstances. In this thesis work, the soil erosion model, Revised Universal Soil Loss Equation (π πππΏπΈ) mingled with the Geographical Information System (πΊπΌπ) tool, has been employed to approximate soil loss under five different scenarios of precipitation products in the Rufiji River Basin situated in Southeastern Tanzania. Remote sensing data can offer the accessibility to quantify the π πππΏπΈ input factors such as rainfall erosivity (π ), Soil erodibility (πΎ), slope length, and steepness (πΏπ), Cover management (πΆ), and erosion control (π) while the areas which are vulnerable to erosion were mapped by πΊπΌπ. The erosivity factor (π ) for the Rufiji river basin was derived from πππ πππ£ππ precipitation and other four different satellite precipitation datasets consisting of twenty years of daily precipitation (1999β2019); The Modern-Era Retrospective analysis for Research and Applications (ππΈπ π π΄β2), Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (ππΈπ ππΌπ΄ππβ πΆπ·π ), Tropical Rainfall Measuring Mission (ππ ππβ3π΅42 π7), and the Global Precipitation Climatology Project (πΊππΆπ). The observed gauged precipitation appeared to be the best dataset since it produced better soil loss and sediment yield assessment results. According to the findings, the Rufiji River basin's overall annual potential soil erosion is estimated to be 1,916,753 t/yr, 863,238 t/yr, 843,069 t/yr, 789,606 t/yr, and 690,625 t/yr based on πππ πππ£ππ precipitation, οΏ½ οΏ½πΈπ π π΄β2, ππΈπ ππΌπ΄ππβπΆπ·π , ππ ππ, and πΊππΆπ respectively. Since the observed data for erosion was unattainable in the Rufiji river basin, the erosion simulation model (π πππΏπΈ) was validated by the concept of sediment delivery ratio applications. The area under low erosion composed of 47.3% in Great Ruaha, 23.5% in Kilombero, 39.5% in Lower Rufiji, and 39.4% in Luwegu Catchment; while the area under very high erosion composed of 7%, 34.2%, 3.5%, and 13.2% in xix Great Ruaha, Kilombero, Lower Rufiji and Luwegu respectively. Around 76.5% of the Rufiji river basin needs abrupt consideration from soil protection experts, especially at Kilombero Catchment. The simulated sediment yield of approximately 1,648,408 t/yr is comparable with the actual sediment of 1,655,056 t/yr; since the sediment delivery ratio was found to be 0.86. The correlation between elected water quality elements, such as πππππ πππππππ¦, πππ, ππ3, ππ», π·π, and sedimentation along water sampling sections was investigated. It was discovered that the sediment yield and water quality parameters have a strong positive relationship. Sediment yield had a strong positive relationship with πππ and π‘π’ππππππ‘π¦ with a correlation of about (0.97). The reliability assessment of global satellite precipitation regarding observed precipitation at the monthly timescale depicted that the ππΈπ π π΄β2 and ππΈπ ππΌπ΄ππβπΆπ·π satellite products perform well regarding π 2, πππΈ, πππ π πππΈ statistics with π 2, πππΈ, and π πππΈ of 0.9, 0.74 πππ 4.2 ππ/ ππππ‘β for ππΈπ π π΄β2, while 0.9, 0.89 and 6.2mm/month for ππΈπ ππΌπ΄ππβπΆπ·π respectively. Generally, the results prescribe that a bulky total of dissipated Soil was discharged from the Rufiji river sanctuary per year. The subsequent sediments normally scaled-down the dam capacity upstream of the basin and might threaten the ecology of the river network. On the grounds of this, it is recommended that the basin requires instant consideration from a soil protection standpoint, particularly in the Kilombero catchment. | en_US |
| dc.language.iso | en | en_US |
| dc.publisher | IIT Roorkee | en_US |
| dc.title | SOIL EROSION MODELLING AND SEDIMENT YIELD FOR RUFIJI RIVER BASIN IN TANZANIA | en_US |
| dc.type | Dissertations | en_US |
| Appears in Collections: | MASTERS' THESES (WRDM) | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| 19548018_Salum Kihiri Reuben.pdf | 7.07 MB | Adobe PDF | View/Open |
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