农业工程学报
農業工程學報
농업공정학보
2014年
4期
230-238
,共9页
王金满%张萌%白中科%杨睿璇%郭凌俐
王金滿%張萌%白中科%楊睿璇%郭凌俐
왕금만%장맹%백중과%양예선%곽릉리
土地复垦%土壤%重构%露天煤矿%多重分形特征%黄土区
土地複墾%土壤%重構%露天煤礦%多重分形特徵%黃土區
토지복은%토양%중구%로천매광%다중분형특정%황토구
land reclamation%soils%reconstruction%opencast coal mine%multi-fractal characteristics%loess area
排土场复垦土壤是由人为方式通过不同重构工艺构成的复杂整体,其由不同颗粒组成、具有不规则形状的特性,其核心工作是重构一个适合植被生长的土壤结构。为了更好地对排土场重构土壤结构进行定量表征,该文通过引入土壤多重分形理论,对山西平朔矿区安太堡露天煤矿排土场4种重构土壤方案(含砾石黄土母质覆盖、含煤矸石黄土覆盖、全黄土母质覆盖、含料姜土黄土覆盖)的2 mm以下土壤粒径分布进行了多重分形参数计算,计算参数包括广义维数谱D(q)、多重分形奇异性指数α(q)以及多重分形谱函数f(α(q))等,并对不同分形参数之间的关系进行了计算。通过研究发现:该研究区大型露天煤矿排土场重构土壤颗粒组成具有明显的多重分形特征, D(0)、D(1)、D(1)/D(0)、Δα和Δf 反映了土壤颗粒分布的非均匀质特征;该研究区黄土重构剖面的土壤粒径分布范围较小、测度集中程度较高、离散程度较小,土壤粒径组成非均匀性低;多重分形参数之间具有较好的相关性,可以简化选择D(0)、D(1)/D(0)和Δα或D(0)、D(1)和Δf 3个参数实现对黄土区重构土壤颗粒组成分布的定量表征;黄土重构剖面0~90 cm内土壤多重分形参数变化明显,黄土区表层土壤覆盖厚度应在90 cm以上,煤矸石和砾石对重构土壤颗粒的离散程度有一定的影响,应排弃在90 cm以下土层。该研究可为黄土区露天煤矿排土场土地复垦以及重构土壤质量的量化提供理论依据。
排土場複墾土壤是由人為方式通過不同重構工藝構成的複雜整體,其由不同顆粒組成、具有不規則形狀的特性,其覈心工作是重構一箇適閤植被生長的土壤結構。為瞭更好地對排土場重構土壤結構進行定量錶徵,該文通過引入土壤多重分形理論,對山西平朔礦區安太堡露天煤礦排土場4種重構土壤方案(含礫石黃土母質覆蓋、含煤矸石黃土覆蓋、全黃土母質覆蓋、含料薑土黃土覆蓋)的2 mm以下土壤粒徑分佈進行瞭多重分形參數計算,計算參數包括廣義維數譜D(q)、多重分形奇異性指數α(q)以及多重分形譜函數f(α(q))等,併對不同分形參數之間的關繫進行瞭計算。通過研究髮現:該研究區大型露天煤礦排土場重構土壤顆粒組成具有明顯的多重分形特徵, D(0)、D(1)、D(1)/D(0)、Δα和Δf 反映瞭土壤顆粒分佈的非均勻質特徵;該研究區黃土重構剖麵的土壤粒徑分佈範圍較小、測度集中程度較高、離散程度較小,土壤粒徑組成非均勻性低;多重分形參數之間具有較好的相關性,可以簡化選擇D(0)、D(1)/D(0)和Δα或D(0)、D(1)和Δf 3箇參數實現對黃土區重構土壤顆粒組成分佈的定量錶徵;黃土重構剖麵0~90 cm內土壤多重分形參數變化明顯,黃土區錶層土壤覆蓋厚度應在90 cm以上,煤矸石和礫石對重構土壤顆粒的離散程度有一定的影響,應排棄在90 cm以下土層。該研究可為黃土區露天煤礦排土場土地複墾以及重構土壤質量的量化提供理論依據。
배토장복은토양시유인위방식통과불동중구공예구성적복잡정체,기유불동과립조성、구유불규칙형상적특성,기핵심공작시중구일개괄합식피생장적토양결구。위료경호지대배토장중구토양결구진행정량표정,해문통과인입토양다중분형이론,대산서평삭광구안태보로천매광배토장4충중구토양방안(함력석황토모질복개、함매안석황토복개、전황토모질복개、함료강토황토복개)적2 mm이하토양립경분포진행료다중분형삼수계산,계산삼수포괄엄의유수보D(q)、다중분형기이성지수α(q)이급다중분형보함수f(α(q))등,병대불동분형삼수지간적관계진행료계산。통과연구발현:해연구구대형로천매광배토장중구토양과립조성구유명현적다중분형특정, D(0)、D(1)、D(1)/D(0)、Δα화Δf 반영료토양과립분포적비균균질특정;해연구구황토중구부면적토양립경분포범위교소、측도집중정도교고、리산정도교소,토양립경조성비균균성저;다중분형삼수지간구유교호적상관성,가이간화선택D(0)、D(1)/D(0)화Δα혹D(0)、D(1)화Δf 3개삼수실현대황토구중구토양과립조성분포적정량표정;황토중구부면0~90 cm내토양다중분형삼수변화명현,황토구표층토양복개후도응재90 cm이상,매안석화력석대중구토양과립적리산정도유일정적영향,응배기재90 cm이하토층。해연구가위황토구로천매광배토장토지복은이급중구토양질량적양화제공이론의거。
Reconstructed soil from an opencast mine dump in a loess area was a complex unity that was made up by humans using different reconstruction technology. It is composed by different soil particles with irregular shapes, and has a self-similar structure. The good soil structure for vegetation growth as reconstructed is the core work of land reclamation. In order to better quantify the soil structure reconstructed in a dump, the soil particle size distribution from four kinds of soil reconstruction modes in the Shanxi Pingshuo ATB Opencast Coal Mine dump was analyzed using the soil multi-fractal theory. Soil reconstruction modes included soil ccovered using loess with gravel, soil covered using loess with coal gangue, covering the whole soil with loess material, and soil covered using loess with Liao Jiangtu. Generalized dimension spectrum D(q), multi-fractal singularity exponentα(q), multi-fractal spectrum function f(α(q)) and other multi-fractal parameters were calculated, and the relationships among the different fractal parameters were analyzed in this paper. The results indicated the following conclusions. (1) The particle distribution of reconstructed soil had significant multi-fractal characteristics in an opencast coal mine dump in the study area. D(0), D(1), D(1)/D(0),ΔαandΔf can reflect the non-uniform particle size distribution characteristics from different perspectives. (2) There was a smaller range of soil particle size distribution, a higher degree of measurement concentration, discrete to a lesser discretization extent, a lower non-uniformity of soil particle size distribution in the soil reconstruction mode of covering the whole loess material, and the function of the mode in changing soil particle size distribution was superior to the modes containing gangue and gravel. (3) The small probability subset of soil particles composition predominated and the soil contained more large particles in the reconstructed soil in the opencast coal mine dump of the loess area. (4) There were good correlations among the multi-fractal parameters of the reconstructed soil particles distribution. D(0), D(1)/D(0) andΔα(or D(0), D(1) andΔf ) can be simplified as three parameters to quantitatively express multi-fractal characterization of the reconstructed soil particle distribution in the study area. (5) The soil multi-fractal parameters in the reconstruction loess section 0-90 cm changed significantly, and the soil thickness covering loess should be more than 90 cm. Gangue and gravel have a certain impact on the dispersion degree of reconstruction soil particles distribution, and should be abandoned in the soil layers below 90cm to reduce its effect on soil particles composition and to improve vegetation restoration .This study can provides a theoretical basis for land reclamation and a quantitative expression of reconstruction soil quality in an opencast coal mine dump of a loess area.