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干旱区地理 ›› 2026, Vol. 49 ›› Issue (3): 559-568.doi: 10.12118/j.issn.1000-6060.2025.225 cstr: 32274.14.ALG2025225

• 生物与土壤 • 上一篇    下一篇

某石化水库植物群丛生物量与不同土层土壤理化性质研究

徐文昭1(), 赵东风1(), 卢磊1, 杜海波2, 赵公大1, 买里旦·莫塔里甫2   

  1. 1.中国石油大学(华东)化学化工学院,山东 青岛 266580
    2.欧赛斯(新疆)科技发展有限公司,新疆 乌鲁木齐 830011
  • 收稿日期:2025-04-22 修回日期:2025-05-28 出版日期:2026-03-25 发布日期:2026-03-24
  • 通讯作者: 赵东风(1968-),男,博士,教授,主要从事化工安全、环保与节能研究. E-mail: zhaodf@vip.sina.com
  • 作者简介:徐文昭(2000-),男,硕士研究生,主要从事石化水库生态环境调查研究. E-mail: xwzzhl@163.com
  • 基金资助:
    新疆维吾尔自治区自然科学基金项目(2024D01B10)

Plant community biomass and soil physicochemical properties at different depths in a petrochemical reservoir

XU Wenzhao1(), ZHAO Dongfeng1(), LU Lei1, DU Haibo2, ZHAO Gongda1, Mailidan MOTALIFU2   

  1. 1. College of Chemistry and Chemical Engineering, China University of Petroleum (East China), Qingdao 266580, Shandong, China
    2. Oasis (Xinjiang) Science and Technology Development Co. Ltd., Urumqi 830011, Xinjiang, China
  • Received:2025-04-22 Revised:2025-05-28 Published:2026-03-25 Online:2026-03-24

摘要:

新疆干旱区某石化企业再生水库由于历史原因在戈壁自然洼地修筑,石化企业将大量的工业废水经过处理以后排入水库形成人工水体,目前水库的建设显著改变了周边荒漠生态系统的土壤-植被关系,形成了独特的湿地景观。以该水库区域内7种典型植物群丛为对象,通过土壤剖面探究不同植被类型下土壤理化性质、碳氮磷化学计量特征及生物量的影响。结果表明:(1)土壤容重随深度显著增大(1.28~1.72 g·cm-3),多枝柽柳-芦苇群丛因放牧及浅根系导致0~60 cm土壤容重最高;土壤含水率呈“表层低-深层高”分布,但研究区域高pH(8.15~8.94)与低阳离子交换量可能引发盐基离子饱和,限制水分可利用性,植被群丛缓解蒸发效应有限;养分(全氮、全磷、有机碳)在表层富集,多枝柽柳群丛固氮能力突出有利于促进氮积累。(2)化学计量特征表明,C:N(6.45~9.07)、C:P(2.77~4.20)和N:P(0.33~0.52)揭示了研究区氮严重匮乏而磷相对富集的失衡状态。(3)多枝柽柳-芦苇群丛单位面积生物量最高(39.67 t·hm-2)且显著优于其他群丛(P<0.05),冗余分析证实全氮(解释度23.4%)、含水率(17.7%)和容重(21.4%)为关键驱动因子。石化水库湿地通过改善土壤-植被关系促进了植被恢复,但盐碱化导致的氮磷失衡与水分可利用性制约着生态功能。因此,生态修复需优先引种耐盐碱固氮植物,优化水分调控。研究结果可为新疆石化企业类似湿地生态修复提供科学范式。

关键词: 石化水库, 干旱地区, 土壤理化性质, 化学计量比, 生物量

Abstract:

A water reservoir had been constructed using a natural depression of the gobi desert—an arid region of Xinjiang, China—for a petrochemical enterprise. The industry discharged large quantities of treated wastewater into the reservoir, forming an artificial water body. This phenomenon created a unique wetland, remarkably altering soil-vegetation relationships within the surrounding desert ecosystem. This reclamation study employed soil profiling to investigate seven plant communities that typically border the reservoir and examine their influence on the soil’s physicochemical properties, including carbon-nitrogen-phosphorus stoichiometry and biomass. The results are summarized as follows: (1) Soil bulk density increased markedly with depth (1.28-1.72 g·cm-3). Such an effect was most prominent within the 0-60 cm layer, induced by a Tamarix ramosissima-Phragmites australis symbiotic association, as these plants were under grazing pressure and had shallow root systems. Soil water content exhibited a “low in surface layers-high in deeper layers” distribution pattern. However, soils with slight alkalinity (pH 8.15-8.94) and low cation exchange capacity across the study area may induce base cation saturation, constraining water availability, a condition exacerbated by the limited abilities of the native vegetation to mitigate evaporation. Nutrient contents—total nitrogen, total phosphorus, and organic carbon—of the surface layer were enriched, as the T. ramosissima-P. australis symbiosis enhanced the nitrogen-fixing capacities of the individual species, facilitating soil nitrogen accumulation. (2) Stoichiometry revealed C:N, C:P, and N:P ratios of 6.45-9.07, 2.77-4.20, and 0.33-0.52, respectively, indicating a severely imbalanced state characterized by nitrogen limitation but relative phosphorus enrichment. (3) The T. ramosissima-P. australis association exhibited the highest biomass per unit area (39.67 t·hm-2), which was significantly greater than that of the other associations (P<0.05). Redundancy analysis identified total nitrogen, soil water content, and bulk density as key driving factors, which explained 23.4%, 17.7%, and 21.4% of the variance, respectively. Thus, the wetlands created by the reservoir facilitated restoration of the native vegetation by improving soil-plant interactions. However, the salinity-induced imbalance in nitrogen-phosphorus stoichiometry and constrained water availability continued to limit ecological functioning. Thus, ecological restoration must prioritize the introduction of salt-tolerant and nitrogen-fixing species as well as optimization of soil water regulation strategies. These results serve as a scientific reference for rehabilitating other petrochemical industrial zones in Xinjiang by creating wetlands.

Key words: petrochemical reservoir, arid region, soil physicochemical properties, stoichiometric ratios, biomass