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Loess Hilly Area area estimation methods
Author: Yuan
Tutor: Yang
School: Inner Mongolia University
Course: Ecology
Keywords: In Loess Hilly Region Valley Surface area Estimate
CLC: S159.2
Type: Master's thesis
Year: 2009
Downloads: 84
Quote: 0
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Abstract
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Different levels, different developmental stages of the valley is an important feature of the loess landscapes. Occurrence, growth and development of the valley and is closely related to the evolution of the Loess Plateau. The formation and development of the valley by the terrain, vegetation, precipitation and other factors, its existence will react on the terrain, vegetation, water, heat and other factors gradually formed intrazonal niche, thus affecting the ecology of the region as a whole process. Due to the the unique landforms structure of the valley of the ups and downs, so study how to efficiently and accurately obtain the actual area of ??the valley (ie the valley of the surface area) urgent need for research work. In this study, by typical watershed in Loess Hilly Region - the Huangfu Hustle domain of typical test area, the Small Watershed Wufendigou high-resolution images and DEM data analysis, simple estimate based remote sensing image valley surface area gully development and the study area as well as the actual valley area of ??the watershed biomass and ecological water a preliminary study, and its structure is as follows: 1. Huangfuchuan watershed, all of the channel can be divided into seven. Relational expressions is more compact, the channel level descending its total length and the channel gully relationship between the number can be represented as: Y 1 = 35.18 * sup > e 0.678x sup>, R 2 sup> = 0.999Y 2 = 0.256 * sup> e 1.568x sup>, R 2 sup> = 0.997 where Y 1 is the total length of a one-channel, the Y- 2 a level valley number, x is the corresponding gully Descending level. The inherent law of gully development of these intrinsic factors is the the estimation formula established by the Institute to be established. 2. Proposed valley area estimation formula based on remote sensing image information: LN (S p ) = 1.012 * sup> LN (L) 5.079LN (S s < / sub>) = 1.012 * sup> LN (L) 5.234-S p for the valley projected area, S s valley surface area, L The gullies length. The derivation of this formula obtained gully surface area estimated coefficient of 1.1677, and the estimate of the surface area of ??gully slope coefficient of 1.2008. Using the estimated coefficients calculate the Huangfuchuan basin surface area than the increase in the projected area of ??276.52 square kilometers. Model application can be used the way of manual identification, extraction of remote sensing image River valley length to estimate the corresponding area of ??the valley. In the case of the degree of crack known basin cutting basin surface area, can be used to estimate coefficient calculation. May be used in the case of a known slope plaque of the projected area of ??the concrete ditch to the surface area of ??the trench slope estimation coefficient calculating the surface area of ??the corresponding plaque. Using established estimating equations with estimated conversion factor, a simple estimation of the vegetation of the study area several main gully slope gully surface area estimates, basin-wide increase in dry matter yield of 19,118.6 tons, ecological water increase of 46.72 million tons, visible ecological effects of the valley is extremely significant.
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CLC: > Agricultural Sciences > Agriculture as the foundation of science > Soil > Soil geography, soil survey > Chinese soil geography, soil survey
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