老万场金矿石灰岩与红土矿体藓类植物生物量及吸水量比较研究

汪文云; 张朝晖

doi:10.3969/j.issn.1001-4810.2009.03.015

老万场金矿石灰岩与红土矿体藓类植物生物量及吸水量比较研究

doi: 10.3969/j.issn.1001-4810.2009.03.015

汪文云¹,
张朝晖²

1.
贵州范师大学生命科学学院
2.
贵州范师大学生命科学学院，贵州省山地环境重点实验室

基金项目: 国家自然科学基金项目(NSFC, No.30860025)、贵州省优秀青年科技人才资助计划项目[黔科合人字（2005）0514号]、国家人力资源和社会保障部留学人员科技活动优秀项目[人社厅（2008）86]

计量
- 文章访问数: 1441
- HTML浏览量: 357
- PDF下载量: 669
- 被引次数: 0
出版历程
- 收稿日期: 2009-05-04
- 发布日期: 2009-09-25

Comparison between biomass and water absorbing capacity of mosses on limestone and lateritic in Laowanchang Lateritic Gold Deposit

WANG Wen-yun¹,
ZHANG Zhao-hui²

1.
School of Life Sciences, Guizhou Normal University,
2.
School of Life Sciences, Guizhou Normal University, Guizhou Provincal Laboratory for Mountainous Environment

摘要

摘要: 长期开采活动使得老万场金矿大量石灰岩出露于地表，区域生态环境严重退化。通过对老万场金矿石灰岩和红土矿体藓类植物优势种类生物量和饱和吸水量进行测定发现：石灰岩表面优势藓类土生对齿藓、小反纽藓、云南墙藓、硬叶对齿藓、芽孢银藓生物量分别高达859、364、292、228、215g/m2，饱和吸水量分别高达1780、9170、1530、2980、2120 g/m2；红土矿体表面优势藓类土生对齿藓、硬叶小金发藓、硬叶对齿藓、梨蒴小毛藓、芽孢银藓生物量分别高达854、596、333、158、134 g/m2，饱和吸水量分别高达3070、10020、1440、1710、4130g/m2。结果显示土生对齿藓在石灰岩和红土矿体表面都是主要的生产者，表现出极强的吸水能力。藓类饱和吸水量与生物量密切相关，生物量较大的藓类植物吸水能力相应较强。特别地，土生对齿藓对该矿区石漠化治理和红土矿体水土保持具有十分重要的现实意义。
- 藓类植物 /
- 生物量 /
- 吸水量 /
- 生态恢复
Abstract: Perennial and devastating mining make a mass of limestone exposed to the earth surface and the eco-environment degraded seriously on Laowanchang gold deposit. After analyzing the biomass and saturated water absorbing capacity of the dominant mosses which are collected from limestone and lateritic gold sites in Laowanchang gold deposit, we have come to the conclusion that, on limestone, Didymodon vinealis (Brid.) Zander, Timmiella diminuta (C.Muell.) P.C.Chen, Tortula yunnanensis P.C.Chen, Didymodon rigidulus Hedw.and Anomobryum gemmigerum Broth. are dominant mosses, with a biomass of 859, 364, 292, 228 and 215g/m2, respectively, and their saturated water absorbing capacity are up to 1 780, 9 170, 1 530, 2 980, 2 120 g/m2, respectively. On ateritic gold sites, Didymodon vinealis Com., Pogonatum neesii Dozy , Didymodon rigidulus Hedw., Microdus brasiliensis (Dub.) Thér. and Anomobryum gemmigerum Broth. are dominant mosses ,with a biomass of 854, 596, 333, 158, 134 g/m2, respectively, and their saturated water absorbing capacity are up to 3 070, 10 020, 1 440, 1 710, 4 130g/m2, respectively. These results show that Didymodon vinealis (Brid.) Zander which owns the largest biomass is the mian preducer on limestone and lateritic gold sites, and its saturated water absorbing capacity is very high too. According to the analysis, it is found that the saturated water absorbing capacity is related to the biomass significantly, which means that the mosses, having large biomass, are able to absorb large quantity of water. Especially, Didymodon vinealis are of important realistic significance to the desertification control in limestone areas and the soil and water conservation in this mine.
- mosses /
- biomass /
- water absorbing capacity /
- eco-rehabilitation

HTML

参考文献(18)

[1]	戴塔根，刘星辉. 我国矿区生态恢复制度几个问题及改进建议［J］.矿冶工程, 2004, 24(5):1-8.
[2]	龙健，黄昌勇，滕应，等. 矿区废弃地土壤微生物及其生化活性［J］.生态学报, 2003, 23(3): 496-504.
[3]	彭少麟.恢复生态学与退化生态系统的恢复［J］.中国科学院院刊，2000，15(3):188 -192.
[4]	彭少麟，赵平，张经炜.恢复生态学与中国亚热带退化生态系统的恢复［J］.中国科学基金, 1999，13(5):279-283.［ 5］ Vitt D H. Patterns of growth of the drought tolerant moss , Racomitrium microcarpon , over a three year period ［J］ .Lindbergia , 1989 ,15 :181 - 187.
[5]	West N E. Structure and function of microphytic soil crusts in wildland ecosystems of arid and semiarid regions ［J］ . Advancesin Ecological Research , 1990 , 20 : 179 - 223.
[6]	Greenfield L E. Retention of precipitation nitrogen by Antarctic mosses ,lichen and fellfield soils［J ］ . Antarctia Science , 1992 , 4 (2) : 205 -206.
[7]	徐杰, 白学良, 田桂泉，等.腾格里沙漠固定沙丘结皮层藓类植物的生态功能及与土壤环境因子的关系［J］.中国沙漠，2005，25（2）：234-242.
[8]	李冰，张朝晖.喀斯特石漠结皮层藓类物种多样性及在石漠化治理中的作用研究［J］.中国岩溶，2009，28（1）：55-60.
[9]	杨元根，刘世荣，金志升.贵州老万场金矿床红土化作用及对金赋存状态的制约［J］. 地球化学, 2004, 33（4）: 414-422.
[10]	王砚耕.贵州西南部红土型金矿成矿背景及其控制因素［J］.贵州地质，1998 15(4): 299 –304.
[11]	任明强.老万场红土型金矿开发与生态环境关系简析［J］.贵州地质，2003，20（2）：117-120.
[12]	徐杰，白学良，杨持，等固定沙丘结皮层藓类植物多样性及固沙作用研究［J］ .植物生态学报，2003，27(4)：545-551.
[13]	Davis R.C. Structure and function of two Antarctic terrestrial moss communities ［J］. Ecol Monogr, 1981, 51: 125-143.
[14]	Leith H. Primary productivity of the major vegetatin units of the world. Ecol Stud, 1975, 14: 203-214.
[15]	Nadkarni NM. Epiphyte biomass and nutrient capital of a neotropical elfin forest［J］. Biotropica , 1984,16 : 249 - 256.
[16]	Silvola J , Aaltonen H. Water content and photosynthesis in peat mosses Sphagnum fuscum and S . angustifolium ［J］. Annual Botany of Fennic , 1984, 21, 1-6 .
[17]	李艳红.苔藓植物的生态生理［A］.吴鹏程.苔藓植物生物学［C］.北京：高等教育出版社，1998，131-147.
[18]	张萍，曾信波.植被蓄水保土功能研究［J］. 山地农业生物学报, 1999, 18（5）: 300-304.