ISSN : 0971-7447
Research Communication
SURFACE FLOW AND SOIL LOSS UNDER DIFFERENT LAND USE CATEGORIES :
A CASE STUDY FROM EASTERN HIMALAYA, ARUNACHAL PRADESH
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R.C. Joshi, Jumri Riba and Tage Rupa
Department of Geography, Rajiv Gandhi University, Rono-Hills Doimukh - 791112, Arunachal Pradesh
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INTRODUCTION Highly fragile and tectonically unstable area with high relative relief and steep slope becomes more vulnerable to soil erosion because of high monsoon precipitation and faulty land use practices. Like other parts of the Himalaya, soil erosion in this area is of major concern and a direct threat to Brahmaputra valley for siltation and resultant floods. Though, it is not possible to stop soil loss completely but, based on the results of the studies, its intensity and amount can be minimized. According to Stoddart (1969), 80% of sediment is reaching to the oceans by the Asian rivers in which Himalayan river are contributing 500-1000 t km-2 yr-1 (Milliman and Meade, 1983). The watershed considered for this study lies in the Lesser Himalayan part of the Arunachal Pradesh. Unscientific intervention adversely affects land degradational processes accelerating the soil loss. The degree and type of vegetation cover are the most important factors in determining rate of erosion (Inbar and Lierena, 2000). Thus, in this study an attempt is made to identify the surface flow and soil loss within different land use categories i.e. agriculture, barren and forest. |
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Figure 1. Location map
STUDY AREA
Upper course of Kale River which forms a wide valley surrounded by hills is delineated as a study area from the SOI topographical map no. 83 E/14 (Fig. 1). It extends in between 27 º 30’ N to 27º 38’N latitude and 93º 45’55”E to 93º 55’ 52”E longitude covering an area of about 207 km2 in Lower Subansiri district of Arunachal Pradesh. Apatani tribe, consisting a population of 27,000 (approximately) inhabits this area (Census-2001).
Using remote sensing data study area is divided into three different land use categories i.e. agriculture, barren and forest. Three erosion plots of a dimension of 3mX5m are established in each land use categories along the 40% slope. The results for the first month of the study were rejected to avoid the effects of the changes resulting from construction of the plots. These plots are fenced with aluminum sheets of 1feet (5 inch is inserted in soil and remaining 7 inch exposed in the air) from all the sides to prevent penetration of water from the adjacent areas. Non recording Rain gauge (Hydromat Make) is installed close to the plots to estimate daily rainfall amount. From each plot surface flow is allowed to be collected in a container through a pipe. Plot wise surface flow and soil loss is estimated for every month. The deposited surface flow in the container is filtered taking sample of one liter (in case overland is below one liter whole amount is taken as sample) water and the material is sorted out. After the completion of filtration, the filter paper with soil is kept for oven dry and the weight of same is measured by digital balance. Present analysis is based on the observations made during May 16th 2005 to May 15th 2006.
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PHYSIOGRAPHY This area forms a typical wide valley, appears to be lacustrine in its origin, in the upper course of the Kale river. A tremendous volume of quaternary unconsolidated sediment derived by erosion of bordering hills found in the study area. The beds of gravel, inter-bedded sand, grit, clay and peat are almost horizontally deposited. The base of the valley is made of gneiss and schist. The altitude of the valley is ranging in between 1540m to 2684m above mean sea level. The relative relief is ranging from level to 520m. The low relative relief is found in and around Hapoli - Ziro locality which falls in the plain area whereas, higher relative relief is found towards the hills. The average slope ranges from level to 28.40. Level slope covers a big patch within the central portion of basin, which is almost flat.Kale River and its tributaries supply water for irrigation and drinking purposes throughout the year. In the rainy season water level becomes very high causing flood along the river course.The weather during summer is pleasant but it becomes severe cold in winter.
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The annual temperature varies from maximum 31˚ c in summer to minimum 0˚ c in winter. The relative humidity use to be more than 90% during rainy season. Due to high rainfall and humidity earth material is weathered very fast in the area. Soils vary from loamy to clayey with a thick layer of humus at the top. In the valley area black and reddish soil is found. Soil acidity ranges from medium to high.
EXISTING LAND USE
Land use and type of management applied to each site explain, to a large extent, the occurrence of the erosion processes (Sanchez et.al.2002). Earlier studies shows that there has been conspicuous land use change in the Himalaya as consequence of population increase and pressure on forest based resources (Rai and Sharma 1998). Thus, a visual interpretation of IRS 1C LISS III FCC and topographical map on 1:50,000 scales is made to delineate land use categories supported by field verification. The identified main land use categories are agriculture, settlement and forest (Fig 3). A brief description of each identified categories is given as below:

The plain area of valley is utilized for wet rice cultivation. Kitchen gardens are very fertile due to continuous application of domestic manure which is used for growing vegetables. The slopes of the adjacent hills in the vicinity of the wet rice-fields are used for rain fed agriculture which includes the production of maize, millet and variety of vegetables. Forest area mainly consists of bamboo and pine trees. In this area people cultivate medium sized straight- stemmed bamboo in close proximity to their villages. Pine is a splendid tree used for timber and firewood purpose. It is grown in the lower slopes of nearby settlement. Most of the bamboo groves are also having scattered pine trees. When pine trees attain height, bamboo do not flourish in the shade of their wide canopy. Besides bamboo and pine, there are number of fruit trees like small cherry, peach, small pear and greenish, bitter apple which are planted in groves, gardens, paths and lanes, burial ground and close to houses. Large number of evergreen as well as deciduous species like hollock, jutuli, tita sopa, hillika, dhuna, borpat, nahar, udal, gonsari, makrisal, bogipoma, khokan, etc. is found in the area. The proportions of evergreen species are more than the deciduous species mainly due to favorable climatic conditions in the area. Plain area of valley is used for agriculture and the slightly elevated areas in the vicinity of flat land are used as settlement. Because of high density of population houses are constructed very closely, mainly built by wooden piles and bamboo. Since long, this area consists seven large villages namely, Hong, Hari, Biila (Reru, Tajang and Kalung), Dutta, Hiija, Mudang-Tage and Bamin-Michi. But due to rapid growth of population (27,000 approx. Census-2001), five more villages are created viz. Siiro, Lempya, Biirii, Nenchachaya and Siibe separating from Hong, Tajang, Mudang-Tage, Dutta & Hiija and Bamin-Michi respectively.
Observation
In comparison to the other parts, the Eastern Himalaya receives heavy rainfall during monsoon. The total rainfall (Fig. 4) is recorded in the study area is 19166 mm, out of which 54.05% is received during monsoon (16th May to 15th Sept). The total wet and dry days (Fig. 5) during monsoon are 64 and 56 respectively with the maximum continuous seven rainy days. Very less rainfall is received with dry days of 54 from (16th Nov. to 15th Aug).
Table 1. Rainfall
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Figure 5. Bar graph showing rainfall chart
The surface flow (Fig. 6) in agriculture, forest and barren is 24482.44 ltr ha-2 yr-1 20996.44 ltr ha-2 yr-1 and 15669.33 ltr ha-2 yr-1 respectively. Maximum surface flow is identified during the 16th July to 15th Aug 2005 because of heavy downpour within a short time. The Minimum surface flow is found during 16th Dec 2005 to 15th Jan 2006 as this time rainfall is very less. Flow under forest cover is directly controlled by rainfall. In general total rainfall amount & intensity and agricultural activities are influencing the total amount of surface flow.
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Figure 6. Bar graph showing Surface flow |
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Table 3. Soil loss
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Figure 7. Bar graph showing soil loss in Agriculture, Barren and forest plot |
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Total annual soil loss (Fig. 7) from agricultural, barren and forest plots is 0.449601 t ha-2 yr-1,0.220779 t ha-2 yr-1 and 0.193212 t ha-2 yr-1 respectively. In agricultural plots (Fig. 8) during 16th June to 15th July and 16th July to 15th August soil loss is observed maximum because of tillage and seed showing in the plot. During these two above mentioned periods of time rainfall intensity was also found very high. During winter, soil loss is almost negligible. In the barren (Fig. 9) and forest (Fig. 10) area soil loss is controlled by the rainfall amount and intensity. Among the all plots minimum soil loss is found in the forest area.
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Figure 8. Agriculture plot and Soil loss
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Figure 9. Barren Plot and Soil Loss
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Figure 10. Forest plot and soil loss
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These observations indicate that under forest cover soil loss and surface flow is very low. Humus contents found in the soil are also highest under the forest as area use to be covered by thick layer of litter. Human disturbed slope (agricultural land) is leading maximum soil loss and surface flow. Depleted forest cover due to deforestation and forest fire in the pine areas appears as grazing land. Because of cool climate regeneration is not very fast. This type of land is considered as barren in which surface flow and soil loss is observed lower than agricultural area. During the observational period of 16th July to 15th August rainfall amount, surface flow, and soil loss is maximum.
ACKNOWLEDGEMENT
G.B.Pant Institute of Himalayan Environment and Development, Kosi, Katarmal, Uttaranchal is duly acknowledged for the generous financial assistance to carry out this work as a part of the research project entitled “Changing land use/Land cover and soil Loss in the Indian Eastern Himalaya, a Drainage Basin input-Output analysis, Arunachal Pradesh. We would like to acknowledge the sincere efforts of Shri Tage Gute for the recording the daily data in the field.
REFERENCE
Luz Amelia Sanchez, Michele Ataroff and Roberto Lopez 2002. Soil erosion under different vegetation covers in the Venezuelan Andes. The Environmentalist, 22, pp 161-172, Netherlands.
Milliman, J.D. and Meade, R.H. 1983. world-wide delivery of river sediment to the oceans, J Geol. 91,1-21.
Moshe, Inbar and Carlos, A Lierena 2000. Erosion processes in High Mountain Agricultural Terraces in Peru. Mountain Research and Development Research and Development vol 20 no 1 00 72-79, USA.
Pande, Anita, Joshi, R.C. and Jalal, D.S. 2002. Selected Landslide types in the Central Himalaya: their relation to geological structure and anthropogenic activities, The Environmentalist Vol 22 pp 269-287, The Netherlands.
Rai, S.C. and Sharma, E. 1998. Comparative assessment of surface flow characteristics under different land use patterns within a Himalayan watershed. Hydrological Processes, 12 pp 2235-2248.
Stoddart, D.R. 1969. World erosion and sedimentation in water in Chorley, R J (ed) water, earth and Man, pp 43-64 Methuen, London.
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