不同植被措施下排土场边坡细沟发育时空特征

为明确不同恢复年限植被措施对煤矿排土场边坡水土流失的防治效应,采用样方调查法,以内蒙古准格尔旗永利煤矿矿区排土场边坡为研究对象,以裸露边坡(CK)为对照,研究不同恢复年限(1a、3a、5 a)的沙柳方格+沙棘+沙打旺(SHA)和沙柳方格+沙打旺(SA)2种措施对细沟发育的影响。结果表明:(1)1a时CK、SHA与SA措施细沟宽度均集中分布在4～8 cm,细沟深度均集中分布在2～4 cm;3 a时CK、SHA与SA措施细沟宽度则集中分布在4～8 cm、8～12 cm、4～8 cm,细沟深度均集中分布在4～6 cm;5 a时CK与SHA措施细沟宽度均集中分布在8～12 cm,而细沟深度则集中分布在4～6 cm和8～14 cm;(2)CK(1～5 a)、SHA措施(1～5 a)和SA措施(1～3 a)的细沟平均宽分别为7.57～11.35 cm、7.58～13.31 cm和5.57～6.14 cm,细沟平均深分别为3.38～6.23 cm、4.19～10.34 cm、2.59～4.24 cm,三者的细沟平均宽深比分别为2.39、2.12和2.05,平均细沟密度分别为1.52～5.25 m·m–2、1.42～1.68 m·m–2和1.88～2.25 m·m–2;(3)1 a时CK、SHA和SA措施的细沟宽深比随坡长变化幅度较大,随着恢复年限增加,宽深比则呈下降趋势,CK、SHA措施和SA措施的细沟密度和细沟侵蚀量均随坡长增加呈增大趋势;(4)与CK相比,1 a时SHA和SA措施边坡细沟侵蚀模数分别减小25.0%和25.86%,两种措施减蚀效果差别不大,而3 a时则分别减小了61.73%和35.31%,SHA措施减蚀效果显著增强。研究结果可以为矿区排土场边坡的植被合理布设提供科学依据与理论指导。     

海州露天矿土地复垦示范区土壤综合质量评价

为有效地治理和改善矿区恶劣生态环境,使废弃的土地资源得以充分利用,通过对阜新海州露天矿土地复垦示范区土壤有机质、全N、有效P、速效K、EC、pH值、含水量、容重、紧实度等指标进行测定,开展了复垦土壤质量综合评价。结果表明:不同复垦示范区土壤质量差异较大,沙打旺、冰草示范区土壤质量最好;杨树、油松示范区次之;耕地、侧柏示范区土壤质量较差。     

露天煤矿排土场植被调查与自然恢复研究(英文)

通过分析辽宁省海州露天煤矿排土场植被组成、物种多样性及重要值的变化,研究了排土场植物群落恢复与演替的一般规律。结果表明:排土场共有植物63 种,分属于23 科,其中菊科15 种、豆科11 种、禾本科8 种;蒺藜+水稗草+猪毛菜、水稗草+大籽蒿+黄蒿、水稗草+披硷草+黄蒿+大籽蒿+黄花草木犀、芦苇+披硷草+水稗草+狗尾草分别是年限为5、10、20、40 梯田层群落的优势种群;重要值对植被重建中物种筛选有指示性,蒺藜在排土场人工恢复中可做为先锋种,披硷草、芦苇、水稗草可做为重要的优势种;排土场植被自然恢复速度缓慢,为了尽快改善生态环境,应该筛选并合理配置先锋植物和适生植物,进行植被重建,加强抚育管理,缩短演替进程。表2 参17。     

乌海市平沟煤矸石山小地形土壤养分分析

文章以乌海市平沟煤矸石山上平台和边坡两种不同小地形上的土壤为研究对象,通过野外调查取样和室内分析化验,研究煤矸石山两种小地形对土壤养分的恢复情况。结果表明,土壤有机质、全N、碱解N含量在两种不同小地形上表现为边坡>平台,土壤P素、K素含量表现为平台>边坡,总体而言,边坡上土壤养分恢复效果比平台好。平台和边坡上土壤养分含量在不同土层深度中均表现为:0~20 cm层>20~40 cm层。通过参考土壤养分分级与丰缺度标准,目前土壤养分丰缺度主要呈现出缺或极缺状态。     

矿区废弃地生态恢复研究进展

就国内外矿区废弃地生态恢复的现状及主要技术问题，包括矿区废弃地基质改良，土壤侵蚀控制，树种选择等进行了讨论。     

Comparison of two methods that assess soil community level physiological profiles in a forest ecosystem

There are currently two approaches that use whole soil to determine community level physiological profiles (CLPP) based on C-substrate utilization. We assessed the Degens and Harris and MicroResp™ approaches for their ability to distinguish between previously mined and non-mined forest soils that are characterized by gradients in biological, chemical and physical properties. Surface soils (0-5 cm) were collected from two ages of forest rehabilitation (3- and 16-years post mining), within mounds and furrows (caused by contour ripping) and from adjacent non-mined forest soil. Microbial respiration response to individual substrates was six times greater from the Degens and Harris (1.84 μg CO₂-C g soil h⁻¹) than the MicroResp™ (0.31 μg CO₂-C g soil h⁻¹) approach. The MicroResp™ approach was able to distinguish between CLPP of the two ages of rehabilitation (P=0.05), whereas the Degens and Harris approach did not. Neither approach identified an overall difference between the CLPP of mined and adjacent non-mined forest. The MicroResp™ approach revealed a significant difference (P=0.03) in CLPP from mounds of the two rehabilitation ages but no differences between the furrows. In addition there was a difference (P=0.03) in CLPP between the mounds and furrows within the 3-year old rehabilitation but no difference between the mounds and furrows within the 16-year-old rehabilitation. However, the CLPP of mounds of the 3-year old rehabilitation were different (P=0.059) to adjacent non-mined forest, while the furrows were not. There was no difference in CLPP between the mounds or the furrows of the 16-year-old rehabilitation and adjacent non-mined forest. These results suggest that the aspect of microbial heterotrophic function measured in this study takes up to 3 years to re-establish in the furrows and between 3-16 years in the mounds of post-mined rehabilitation soils. Our results also indicated that the MicroResp™ was substantially better than the Degens and Harris approach in distinguishing between treatments; this is likely to be due to differences in substrate concentrations and soil water potentials between approaches. Testing of a more comprehensive range of organic compounds would likely provide greater ecological interpretation of the CLPP data.     

Dynamics of microbial biomass and nitrogen supply during primary succession on blastfurnace slag dumps in dry tropics

This paper reports the role of microbial biomass in the establishment of N pools in the substratum during primary succession (till 40-year age) in Blastfurnace Slag Dumps, an anthropogenically created land form in the tropics. Initially in the depressions in the slag dumps fine soil particles (silt+clay) accumulate, retaining moisture therein, and providing microsites for the accumulation of microbial biomass. In all sites microbial biomass showed distinct seasonality, with summer-peak and rainy season-low standing crops. During the summer season microbial biomass C ranged from 18.6 μg g⁻¹ in the 1-year old site to ca. 235 μg g⁻¹ in the 40-year old site; correspondingly, microbial biomass N ranged from 1.22 to 40 μg g⁻¹. On sites 2.5-years of age and younger, the microbial biomass N content accounted for more than 50% of the organic N in the soil, whereas the proportion of microbial biomass N was ca. 7% of organic N in 40-year old site. The strong correlation between microbial biomass and total N in soil indicated a significant role of microbes in the build-up of nitrogen during the initial stages of succession in the slag dumps. Though the organic N pool in the soil was low (594 mg kg⁻¹) even after 40 years of succession, the available N (NH₄-N and NO₃-N) contents in the soil were generally high through the entire age series (ca. 16-32 μg g⁻¹) during the rainy season (which supports active growth of the herbaceous community). The high mineral-N status on the slag dump was related with high N-mineralization rates, particularly in the young sites (20.6 and 13.9 μg g⁻¹ month⁻¹ at 1 and 2.5-year age). We suggest that along with the abiotic factors having strong effect on ecosystem functioning, the microbial biomass, an important biotic factor, shows considerable influence on soil nutrient build-up during early stages of primary succession on the slag dumps. The microbial biomass dynamics initiates biotic control in developing slag dumps ecosystem through its effect on nitrogen pools and availability.     

德兴铜矿尾矿库植被重建后的土壤肥力状况和重金属污染初探

德兴铜矿是我国的超大型铜矿,尾矿砂的排放是其主要的环境问题之一,目前主要堆积于尾矿库中。1号尾矿库于1986年服役期满后共堆积矿砂2.15×107 m3,面积约210 hm2。20世纪90年代后期,在坝坡约30 hm2覆有客土的地区进行了一系列植被重建的试验研究工作,本文报道了1998年开始在旱稻(OryzaLinn.)、花生(Arachis Linn.)、香根草(Vetiveria zizanioidesNash)和湿地松(Pinuselliottii Engelm.)等18种不同植被组合条件下的土壤基本农化性状(pH、有机质(OM)、铵态氮、速效P、速效K)以及0.05 mol L-1 HCl可提取态重金属在3~4年时间内的变化情况,结果表明,坝坡土壤N、P、K严重不足,且保水、保肥能力弱,需要不断地进行培肥和改良。三年多来,土壤pH总体上无显著变化;OM第三年有显著上升,约为第一年的127%;NH4 N成直线下降,第二年和第三年分别为第一年的72.9%和43.0%;随着耕作实践的推移,速效P和速效K显著上升,但仍旧处于较低水平。重金属(主要是Cu)污染严重,Cu、Zn、Pb、Cd在植物中有明显积累。研究结果强调了试验区在植被重建中不宜种植食用植物,以避免食物链的污染。     

Soil respiration on reclaimed coal-mine spoil

Summary Measurements of soil respiration were made at a number of soil-covered reclaimed coal-mine spoil sites. Many chemical and physical soil factors likely to affect the respiration were also measured. A combination of principal component, cluster, and multiple regression analyses was used to indicate the important factors. These were found to be water-holding capacity and organic matter content. In some cases soil pH was also a controlling factor.     

抚顺西排土场矸石山阴坡物种多样性变化特征

抚顺西排土场矸石山阴坡随着排矸年限的增加，物种多样性发生变化，物种数由初期的4科5种增至后期14科29种。植被由最初的鹅绒藤＋豚草＋刺蒺藜群落，逐步演变到榆树群落。在阴坡，不同排矸年限的样地，植物群落多样性指数随着排矸时间的延长而增加；物种综合多样性指数、丰富度指数与排矸年限呈显著正相关关系。