Nutrient Mineralization and Leaf Litter Preference by the Earthworm Pontoscolex corethrurus on Iron Ore Mine Wastes

Abstract The effects of the earthworm Pontoscolex corethrurus (Muller) on the rate of mineralization of cattle dung‐amended iron (Fe^{2 +} ) ore mine wastes and its preference for partially decomposed leaf litter with contrasting chemical composition were studied in pot trials. The growth and survival rates of earthworms showed significant positive correlations with percent of organic matter. During 96 days of exposure, the earthworms significantly increased exchangeable Ca^{2 +} , Mg^{2 +} , PO₄^{3 ?} and NH₄‐N. Iron ore mine wastes amended with 5–10% organic matter supported earthworm fauna better than mine wastes amended with 0–3% organic matter. The leaf litter preference shown by the earthworm was, in descending order, Phyllanthus reticulatus, Tamarindus indica, Anacardium occidentale, Casuarina equisetifolia, Acacia auriculiformis, and Eucalyptus camaldulensis. A significant positive correlation was observed between the survival and growth rates of earthworms and the nutrient contents of partially decomposed leaf litter. The first three plant species were significantly richer in nutrients, mainly organic carbon, calcium, phosphorus, and nitrogen, than the other two plant species. Acacia auriculiformis and E. camaldulensis litter were preferred less because of their high lignin and polyphenolic compounds, despite being rich in other macronutrients like nitrogen and phosphorus. It is concluded that the introduction of P. corethrurus to cattle dung‐amended (5–10%) iron ore mine wastes or revegetation of the sites with P. reticulatus, T. indica, and A. occidentale plant species should be attempted before earthworm introduction. The litter from these species acts as a source of food for earthworms, thereby hastening the process of restoration of abandoned iron ore mines of Goa, India.     

围栏禁牧对滇西北高寒湿地土壤活性有机碳的影响

过度放牧导致滇西北高寒湿地碳汇功能逐渐丧失,围栏禁牧作为一种有效的湿地恢复方式,其对滇西北高寒湿地土壤碳库的影响尚缺乏研究。为探明围栏禁牧对滇西北高寒湿地土壤活性有机碳的影响,以纳帕海湿地不同禁牧年限(未禁牧、禁牧3年、禁牧8年、禁牧10年)的草甸和沼泽化草甸作为研究对象,对比分析不同禁牧年限草甸和沼泽化草甸土壤总有机碳(TOC)、颗粒有机碳(POC)、溶解性有机碳(DOC)、易氧化有机碳(EOC)和微生物生物量碳(MBC)含量特征。研究结果表明,随着禁牧年限的增加(<10 a),草甸和沼泽化草甸土壤TOC、DOC、EOC、MBC含量显著增加(P<0.05);随着土壤深度的增加,草甸和沼泽化草甸土壤TOC、EOC和MBC含量逐渐下降,而POC和DOC含量逐渐增加。土壤理化性质显著影响土壤活性有机碳各组分含量,其中总氮(TN)是影响草甸和沼泽化草甸土壤活性有机碳各组分含量的主导因素。围栏禁牧有利于滇西北高寒湿地土壤质量和固碳能力的恢复,且随着禁牧年限的增加,恢复效果越明显。相同恢复年限,纳帕海沼泽化草甸土壤恢复效果比草甸土壤显著。研究可以为放牧湿地恢复研究提供理论基础。     

Fifteen Years of Vegetation and Soil Development after Brackish-Water Marsh Creation

Aboveground biomass, macro‐organic matter (MOM), and wetland soil characteristics were measured periodically between 1983 and 1998 in a created brackish‐water marsh and a nearby natural marsh along the Pamlico River estuary, North Carolina to evaluate the development of wetland vegetation and soil dependent functions after marsh creation. Development of aboveground biomass and MOM was dependent on elevation and frequency of tidal inundation. Aboveground biomass of Spartina alterniflora, which occupied low elevations along tidal creeks and was inundated frequently, developed to levels similar to the natural marsh (750 to 1,300 g/m²) within three years after creation. Spartina cynosuroides, which dominated interior areas of the marsh and was flooded less frequently, required 9 years to consistently achieve aboveground biomass equivalent to the natural marsh (600 to 1,560 g/m²). Aboveground biomass of Spartina patens, which was planted at the highest elevations along the terrestrial margin and seldom flooded, never consistently developed aboveground biomass comparable with the natural marsh during the 15 years after marsh creation. MOM (0 to 10 cm) generally developed at the same rate as aboveground biomass. Between 1988 and 1998, soil bulk density decreased and porosity and organic C and N pools increased in the created marsh. Like vegetation, wetland soil development proceeded faster in response to increased inundation, especially in the streamside zone dominated by S. alterniflora. We estimated that in the streamside and interior zones, an additional 30 years (nitrogen) to 90 years (organic C, porosity) are needed for the upper 30 cm of created marsh soil to become equivalent to the natural marsh. Wetland soil characteristics of the S. patens community along upland fringe will take longer to develop, more than 200 years. Development of the benthic invertebrate‐based food web, which depends on organic matter enrichment of the upper 5 to 10 cm of soil, is expected to take less time. Wetland soil characteristics and functions of created irregularly flooded brackish marshes require longer to develop compared with regularly flooded salt marshes because reduced tidal inundation slows wetland vegetation and soil development. The hydrologic regime (regularly vs. irregularly flooded) of the “target” wetland should be considered when setting realistic expectations for success criteria of created and restored wetlands.     

湿地生态单元定义及其在湿地恢复中的应用

生态单元的概念在生态系统的环境保护和生物保护中被广泛应用。通过阐述湿地生态单元的定义、内涵和外延,分析了湿地生态单元的特征,介绍了湿地生态系统的内部生态单元、湿地\"外援\"生态单元和人工重建湿地生态单元等在湿地恢复中的应用案例,并对湿地生态单元未来需要关注的研究方向进行了总结,以期为湿地保护与精细化管理提供理论基础和科学依据。     

自然湿地生态恢复研究综述

湿地由于具有丰富的资源、独特的牛态结构和功能而享有“自然之肾”之称。为了更好地保护和开发利用湿地,世界各国都在积极采取措施阴止湿地的退化或消失,湿地的生态恢复与重建问题已成为生态学和环境科学的研究热点,在全面综述国内外湿地生态恢复研究进展的基础上,对湿地乍态恢复研究的重点和热点进行了探讨和分析,指出我国为做好湿地生态恢复工作尚需进一步加强湿地生态恢复的方法学、基础理论、应用技术和示范推广等方面的研究。     

表土在日本植被恢复中的应用

土壤种子库具有区域特有的物种组成和遗传特性,对维持物种多样性和种群密度起到重要作用.表土是具有植被恢复潜在能力的绿化材料.本文在参考大量日本文献的基础上,介绍了利用表土进行植被恢复的特点及分类,从表土混合比例、坡面环境、表土采集深度等3个方面归纳分析了利用表土进行植被恢复的方式,介绍了其在森林、道路、湿地、废弃地等不同类型生境中的应用.最后针对表土在植被恢复应用中存在的问题提出了今后的研究课题:应加强表土在植被恢复中的应用研究,明确绿化技术、恢复目标及表土作为绿化材料的适用性调查方法和标准,开发低成本、高效率的新型表土利用方法.     

The effect of concentrated smoke products on the restoration of highly disturbed mineral sands in southeast Victoria

Summary Recent studies have recognized the potential of broad‐scale surface application of smoke compounds for enhancing germination from the soil seed‐bank in fire‐prone vegetation communities. Results suggest that smoke technology may play, in the future, a significant role in the restoration and management of areas supporting indigenous vegetation. An important step in the development of smoke‐based restoration tools is the conduct of in situ field trials in a range of geographical locations and environmental conditions. However, most of the published work on the effectiveness of smoke products in promoting seedbank germination has been conducted at sites in southwestern Australia. The present study examines the effect of commercially available smoke‐water products on the regeneration of a highly disturbed former mine‐site at the Royal Botanic Gardens Cranbourne, in southeastern Victoria. Various combinations of concentrated smoke products and topsoil harvested from a nearby heathy woodland community were applied to exposed, uniform mineral sands to test their effect on seedling density and species richness of regrowth. The trials showed that after 12 months a number of common, herbaceous species including Austrodanthonia setacea, Opercularia varia and Platysace heterophylla were recorded in significantly higher numbers in areas treated with a commercial smoke‐water. However, there was no overall improvement in the density of seedlings or the richness of species as a result of the application of the smoke products. Similarly, total seedling density and species richness were not affected by the addition of topsoil, either alone or in combination with smoke products.     

Can Carbon and Phosphorous Amendments Increase Native Forbs in a Restoration Process? A Case Study in the Northern Tall‐grass Prairie (U.S.A.)

In the northern Great Plains (United States), sites with less than 20% of native species are difficult to restore. We have experimented with a restoration method that shows some promise. It consists of systematically installing simulated small‐scale patches (8.0 m² in size) over 25% of an old field and then seeding these patches with native species. The working hypothesis is that these patches will generate a constant source of propagules which in time will lead to increases in native species diversity within the surrounding grass matrix. The objective of this paper was to determine whether soil amendments should be used to facilitate the establishment and persistence of native species (primarily forbs) within these patches. We seeded the patches with a mixture of native grass and forb species and applied four soil treatments: P fertilization, C additions, C + P, and a control (no amendments). Results for the first 5 years were as follows: (1) seeded forb richness was mostly unaffected by soil amendments; (2) seeded and nonseeded forb biomass and density were substantially reduced by C additions, whereas they were unaffected or increased under P additions; (3) both seeded and non‐native grass biomass substantially increased with C additions; and (4) there was an inverse relationship between native seeded forbs and non‐native grass biomass. Our conclusions are that: (1) P amendments are a potential tool for enhancing native seeded forb biomass in simulated small‐scale disturbance patches; and (2) C additions, although enhancing seeded grass biomass do not reduce the biomass of non‐native grasses.     

Diary

Abstract

The use of organic amendments is a common practice in Pakistan to improve soil fertility. Organic amendments affect the chemical speciation and thus the bioavailability of heavy metals and their uptake and toxicity to plants. The present study evaluates the influence of organic amendments viz. farm yard manure (FM), poultry manure (PM), press mud (PrM) and activated carbon (AC) on nickel (Ni) bioavailability in soil, as well as its uptake into, and growth responses of, Trifolium alexandrinum. Pot experiments were conducted where T. alexandrinum was exposed to three different concentrations of Ni i.e., 30, 60 and 90 mg kg^?1 in the form of NiCl₂ solution in the presence and absence of organic amendments each applied at 15 g kg^?1 soil. The results showed that the effect of organic amendments on Ni bioavailability and uptake by T. alexandrinum depended on the Ni concentration in the soil and the amendment type. Application of organic amendments generally increased Ni phytoavailability in soil and Ni uptake by plants at low Ni levels (Ni-0 and Ni-30) but decreased at higher levels (Ni-60 and Ni-90).     

表土在彭湖高速公路低缓边坡生态恢复中的应用

选取江西省彭泽至湖口高速公路沿线5个典型低缓边坡试验点,利用表土生态恢复,采用样线法调查1年后的试验边坡植物的生长情况。结果表明:在彭湖高速公路低缓边坡利用表土资源进行边坡生态恢复是可行的,各种利用表土的试验设计均取得了较好的恢复效果,其中,边坡覆盖7～10cm中层厚度表土后采取人工撒播恢复方式,边坡植物群落的Simpson多样性指数(平均0.80)及Pielou均匀度指数(平均0.84)相对较高,恢复效果较好;同时,此试验条件下生物量的积累值(平均446g.m-2)和木本植被的群落重要值(平均14.5)都显著高于其他恢复方式,这有利于群落结构的稳定和延续。     

湿地生态系统健康研究进展

湿地作为一个生态系统 ,具有多种功能和价值 ,是人类最重要的环境资本之一 ,被称为“自然之肾”。湿地在蓄洪防旱、调节气候、控制土壤侵蚀、促淤造陆、降解环境污染等方面起着极其重要的作用。湿地拥有丰富的野生动植物资源 ,是众多野生动植物特别是珍稀水禽的繁殖和越冬地。不仅如此 ,湿地向人类提供大量的生产和生活资料 [1] 。然而 ,近些年来一些地区的湿地状况令人担忧 ,具体表现城市化、工业化、路基建设、农业开发及废物处理等造成湿地面积的缩小 ;水利、灌溉、水库蒸发、河流及地下水过度提取 ,沼泽地排水、挖渠、土地开荒、筑堤造…     

Comparison of Soil Organic Matter in Created, Restored and Paired Natural Wetlands in North Carolina

Soil organic matter (SOM) content is a key indicator of soil quality and is correlated to a number of important soil processes that occur in wetlands such as respiration, denitrification, and phosphorus sorption. To better understand the differences in the SOM content of created (CW), restored (RW), and paired natural wetlands (NWs), 11 CW/RW-NW pairs were sampled in North Carolina. The site pairs spanned a range of hydrogeomorphic (HGM) subclasses common in the Coastal Plain. The following null hypotheses were tested: (1) SOM content of paired CW/RWs and NWs are similar; (2) SOM content of wetlands across different HGM subclasses is similar; and (3) interactions between wetland status (CW/RW vs. NW) and hydrogeomorphic subclass are similar. The first null hypothesis was rejected as CW/RWs had significantly lower mean SOM (11.8 ± 3.9%) than their paired NWs (28.98 ± 8.0%) on average and at 10 out of the 11 individual sites. The second and third null hypotheses were also rejected as CW/RWs and NWs in the non-riverine organic soil flat subclass had significantly higher mean SOM content (31.08 ± 14.2%) than the other three subclasses (8.18 ± 2.5, 11.18 ± 8.2, and 10.38 ± 4.2%). Individual sites within this fourth subclass also had significantly different SOM content. This indicated that it would be inappropriate to include the organic soil flat subclass with either the riverine or non-riverine mineral soil flat subclasses when considering restoration guidelines. These results also suggested that if there is a choice in mitigation options between restoration or creation, wetlands should be restored rather than created, especially those in the non-riverine organic soil flat subclass.     

Influence of physical processes on the design, functioning and evolution of restored tidal wetlands in California (USA)

The performance of two intertidal wetland mitigation projects constructed by the California Department of Transportation (Caltrans) in the Sweetwater Marsh National Wildlife Refuge (SMNWR) in San Diego Bay was evaluated over 5 years. Most of the Sweetwater wetland complex has been altered this century, including diking (with subsequent subsidence), filling, modification of the tidal regime, freshwater inflow and sediment fluxes. The mitigation project goals included a range of functional criteria intended to support two endangered bird species (light-footed clapper rail and California least tern) and one endangered plant (salt marsh bird's-beak). While the mitigation projects have achieved some of the performance criteria established in the regulatory permits (particularly, those related to fish), vegetation criteria for one of the bird species have not been met. The initial grading (in relation to local tidal datums) should support the target plant species, but growth has been less than required. Shortcomings of the habitat include elevated soil and groundwater salinity, low nutrient levels (especially nitrogen, which is readily leached from the coarse substrate), and eroding topography (where a single oversized and overly sinous channel and the lower-than-natural marshpalin result in high velocity surface water flow and erosion). The failure to achieve a large plain at low-marsh elevations highlights the importance of a more complete understanding of the relationship between the site physical processes (topography, hydrology, climate, geomorphology), substrate conditions, and biotic responses.Corresponding editor: R.E. Turner