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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B8, 2012
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia
2. METHODS
2.1 Study area
The Phewa lake watershed area is located in the
south-west corner of the Pokhara valley (28°7
N to 28712/N latitude and 84^5^E to 84°10" E
Longitude) which lies on a relative subsidence
zone between the greater Himalaya and
Mahabharat range. This watershed is spread
fully or partially of six VDCs (Sarangkot,
KaskiKot, Dhikurpokhari, Bhadaure Tamagi,
Chapakot and Pumdi Bhumdi) and the
southwestern part of the Pokhara sub-
metropolitan city of Kaski district. It covers an
area of Approximately 123 km? and the length
and width of the east-west oriented watershed
is about 17 and 7 Km respectively. The surface
area of the Phewa Lake is 4.43 km^ and depth
from 8.6m to 19 m. The watershed height
varies from lower part from sea level 793m to
the upper part 2508m. The mean annual rainfall
in the study area for the past 10 years from
2001 to 2010 is 4325.75mm. More than 80%
of the annual rainfall occurs during the
monsoon season in the months of June to
September. The months from October through
May are generally very dry season. The study
area is the representation of the hill region of
Nepal The study area has the scattered
settlement with different casts.
2.2 Survey methods
Socio economic data were obtained from the
village profile of village development
committee report published in 2010 and the
questionnaire survey carried out from the
different stakeholder’s from the watershed area.
The report of the village profile contained data
of whole study area of the Phew watershed
including the number of house, the number of
families, income of the families, land use and
land cover in the study area. The questionnaire
Survey was conducted to evaluate the impact of
soil erosion due to the socio economic, climatic
and anthropogenic factors. 310 questionnaires
were collected from the 14-sub watershed area
of stakeholders like farmers, mothers’ group,
teachers, social workers, NGO/GO officers,
politicians, students etc. The data collected was
based on individual interviews, focus group
discussion key informant interviews and field
observation method were using questionnaire to
investigate for the socio-economic and climatic
and anthropogenic factors. The primary
information derived from the questionnaire
surveyed was climatic, anthropogenic and
socioeconomic factors. Garmin GPS collected
GPS points of the household. The collected
points were projected to the map of the study
area. Data on average rainfall, humidity and
temperature were collected from the relevant
government agencies and meteorological
department government of Nepal. These
climatic data were compared with soil erosion
of the study area.
Primary data were collected from a field
survey. A structured questionnaire composed of
12 Variables, all potentially influencing for the
soil erosion were designed to obtain the
information from the personal interview and
discussion with all types of stakeholders’. The
questionnaire collected data about the soil
erosion details were interviewed.
Secondary data including demographic
information about the Phewa watershed area
such as rainfall, temperature and the list of soil
erosion from the watershed area were analyzed.
The soil erosion data were collected from the
Government office NGO and the village
development committees. The broad structured
questionnaires were used for the personal,
social, economical, resources management,
climatic and participatory approach for soil
conservation practices. Additional qualitative
information such as change in soil conservation
practices, role of local level institution
initiation, land management practices six focus
group discussions in six VDC, 12 key
informant interviews and through the
observation of the watershed. Focus group
discussions were conducted between the
stakeholders’ farmer, teacher, politician,
mothers’ group member and NGO/GO officers,
students. A checklist was prepared for the
discussion, a researcher was facilitated in