农业工程学报
農業工程學報
농업공정학보
2014年
1期
236-244
,共9页
杨翠霞%赵廷宁%谢宝元%曹福存%张成梁%张艳
楊翠霞%趙廷寧%謝寶元%曹福存%張成樑%張豔
양취하%조정저%사보원%조복존%장성량%장염
土地复垦%地貌形态%矿区%流域%重塑%地貌系统信息熵
土地複墾%地貌形態%礦區%流域%重塑%地貌繫統信息熵
토지복은%지모형태%광구%류역%중소%지모계통신식적
land reclamation%geomorphology%mines%watershed%reconstruction%geomorphic information entropy
地貌重塑是废弃矿区土地复垦与生态重建的重要基础部分和重点研究的技术问题之一。该文根据流域地貌学及其自相似原理,利用 ArcGIS 技术重新规划了废弃矿区的子流域及沟道、计算了矿区邻近未干扰子流域地貌形态特征数据并作为参照的标准;在此基础上结合 Geofluv 模型重建了北京市房山区黄院废弃采石场的小流域地貌,探讨了基于小流域自然形态的废弃矿区地貌重塑原理与技术方法,分析了重塑后的与未干扰的子流域形态特征间关系。结果表明,重塑后子流域地貌形态是相对稳定的、自然的,并与未干扰的子流域形态特征比较相似;用地貌系统信息熵值判断出重塑后地貌起伏变化小,受侵蚀强度弱,水土流失趋向于非常缓和。该文研究成果为废弃矿区地貌重塑的研究提供了一种新思路。
地貌重塑是廢棄礦區土地複墾與生態重建的重要基礎部分和重點研究的技術問題之一。該文根據流域地貌學及其自相似原理,利用 ArcGIS 技術重新規劃瞭廢棄礦區的子流域及溝道、計算瞭礦區鄰近未榦擾子流域地貌形態特徵數據併作為參照的標準;在此基礎上結閤 Geofluv 模型重建瞭北京市房山區黃院廢棄採石場的小流域地貌,探討瞭基于小流域自然形態的廢棄礦區地貌重塑原理與技術方法,分析瞭重塑後的與未榦擾的子流域形態特徵間關繫。結果錶明,重塑後子流域地貌形態是相對穩定的、自然的,併與未榦擾的子流域形態特徵比較相似;用地貌繫統信息熵值判斷齣重塑後地貌起伏變化小,受侵蝕彊度弱,水土流失趨嚮于非常緩和。該文研究成果為廢棄礦區地貌重塑的研究提供瞭一種新思路。
지모중소시폐기광구토지복은여생태중건적중요기출부분화중점연구적기술문제지일。해문근거류역지모학급기자상사원리,이용 ArcGIS 기술중신규화료폐기광구적자류역급구도、계산료광구린근미간우자류역지모형태특정수거병작위삼조적표준;재차기출상결합 Geofluv 모형중건료북경시방산구황원폐기채석장적소류역지모,탐토료기우소류역자연형태적폐기광구지모중소원리여기술방법,분석료중소후적여미간우적자류역형태특정간관계。결과표명,중소후자류역지모형태시상대은정적、자연적,병여미간우적자류역형태특정비교상사;용지모계통신식적치판단출중소후지모기복변화소,수침식강도약,수토류실추향우비상완화。해문연구성과위폐기광구지모중소적연구제공료일충신사로。
Topographic reconstruction is a crucial part of land reclamation and ecological rehabilitation because the resulting geography landscapes are the foundations for all subsequent reclamation practices and the surfaces for future land uses. It is also ranked among the most important research technical problems. Nature can provide analogues for mined or mining landscapes during disturbed-land reclamation according to landscape stability and according to the reconstructed structure blending in with the surrounding undisturbed landscape. In terms of the watershed geomorphology and the principle of self-similarity theory, the sub-catchments and channels of abandoned mines were re-planned by using ArcGIS soft technology and a practical survey in this paper. At the same time, the topography characteristics of adjacent, undisturbed catchments were calculated by applying an ArcGIS Hydrologic analysis tool, which was taken as the following simulation reference standard. Then the topography in a sub-watershed unit in the Huangyuan abandoned quarry project of Fangshan county in Beijing city was reconstructed by using a Geofluv (Natural Regrade) module driven by geomorphic principles, in which this module simulated the function of the natural landscape that would evolve over time under the physical and climatic conditions present at the site to water and sediment from the land surface in a stable hydrologic equilibrium. Moreover, the theory and technical method of the reconstructed topography were studied. The initial study of the sub-watershed on the undisturbed landform in the project’s vicinity were selected and calculated to develop a stable channel design and reconstruction guidelines by using GIS spatial analysis tools, and the selected geomorphologic characteristics index were first and second order sub-watershed, the average sub-watershed area, main channel, drainage density, watershed roundness, average elevation difference, and average slope, which provided targets for topographic reconstruction. In this case, the average second order drainage density that represented the stable sub-watershed size for the local condition was 13.84km/km2. Moreover, the average second order drainage density of the reconstructed topography which simulated the natural landform evolution to the stage in balance with the local environmental condition was 14.52km/km2 on the basis of a re-planning of reconstruction sub-watershed and main channel, which achieved the desired design goals. The results showed that the reconstructed Huangyuan topography in which the hydrologic and fluvial geomorphic analyses and stable channel parameters were determined, and based on site-specific data, were relatively economical, stable, and natural, which was similar to the undisturbed catchments’ geomorphology. Finally, the relationship of geomorphologic characteristics between the reconstructed sub-watershed and the undisturbed ones was analyzed and the ratio of the index was almost similar. A topographic reconstruction simulated a relatively stable sub-watershed performed by geomorphic processes with the creation of a basin composed of slope and channels in orderly spatial arrangements and functioning for the transportation of water and sediment. The geomorphic information entropy analysis showed that the geomorphology changed very slowly after topographic reconstruction and the erosions on watershed were also gradually reduced. This study provided a novel viewpoint for the topographic reconstruction of an abandoned mine.