Page 8 - ต้นแบบอนุรักษ์ดินและน้ำจังหวัดเชียงใหม่ Soil and Water Conservation Model in Chiang Mai Province.
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                                                            Abstract


                          From October 2015 to September 2020, the Paired Watershed project was implemented

                   in the Mae Poi and Huai Luek sub-basins of Chiang Dao district in Chiang Mai  Province. The

                   standard soil erosion plot sites are 4 x 22 meters in size and are installed in three slope classes:
                   9-10 percent, 20-25 percent, and 30-35 percent. Both sub-basins are made up of six parcels of

                   land that are used differently. The objective is to assess the impact of soil erosion using an
                   empirical aspect mathematics equation and MMF soil erosion modeling.


                          At Mae Poi and Huai Luek sub basins, the maximum average annual rainfall was 5,297.60

                   mm in 2017, whereas the lowest average annual rainfall was 1,085.60 mm in 2020. Huai Luek sub

                   basin has a greater quantity of soil sediment box than Mae Poi sub basin, which has 2,357.87
                   kg/rai or soil erosion class 0.79 ton/rai/year and Mae Poi sub basin has 1,912.68 kg/rai or soil

                   erosion class 0.79 ton/rai/year. The greatest soil sedimentation rate in a vegetable plot is 1.17

                   ton/rai/year.  The  natural  Mixed  Deciduous  Forest,  on  the  other  hand,  has  the  lowest  soil
                   sediment level at 0.27 ton/rai/year. In addition, the mathematics equation generates a soil erosion

                   class of 0.20 ton/rai/year, as defined by the Land Development Department in 2013. Furthermore,

                   MMF modeling predicts 3.05 tons per rai per year in the Mae Poi sub-basin and 1.78 tons per rai
                   per year in the Huai Luek sub-basin. According to the following, the MMF model's soil erosion

                   evaluation  includes  both  empirical  and  mathematical  equations  of  soil  erosion  in  the  same
                   direction.
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