近50年来河西走廊区域生态环境变化特征与综合防治对策

近50年来,河西走廊地区在人类活动强烈作用和区域气候变化双重驱动下,区域水文与生态环境发生了一系列变化。①区域出山径流过程表现为走廊东段的石羊河流域出山流量多年变化呈显著减少趋势,河西走廊中、西段的黑河流域和疏勒河流域年均出山流量则呈现递增趋势,但下游河流水量锐减并呈现明显的人为水文过程特征,水体盐化和污染趋势加剧,其中Ⅳ～Ⅴ级污染河道长度达到208km。②南部祁连山区森林面积减少约16.5%,自20世纪90年代以来逐渐有所恢复;北部天然荒漠森林则持续衰退,天然林加速消亡,仅额济纳和民勤两地减少林地34.31×104hm2。草地生态呈现以面积减少、草地荒漠化和载畜能力降低等为特征的持续退化趋势,河西地区总体退化草地面积达46.86%。③近50年来河西土地沙漠化发展十分强烈,其发展速度在80年代初期最高达到年递增2.15%,80年代后期至90年代,全区域土地沙漠化过程出现明显的减缓。以流域为单元,进行水资源统筹利用规划与管理,统筹兼顾不同区域经济发展与生态环境建设对水的需求,以生态系统健康发展为原则,遵循生态规律来进行土地资源的开发利用,系统开展流域为单元的生态功能保护与建设是提高区域可持续发展能力的根本途径。

Salt-Water Dynamics in Highly Salinized Topsoil of Salt-Affected Soil During Water Infiltration

Continuous monitoring of salt and water movement in the soil profile of highly salinized topsoil under steadystate infiltration was conducted.It gives that salt and water dynamics during convection-diffusion period can be divided into three stages:1.formation of a salt peak,2.the salt peak moving downwards till the appearance of the summit of the salt peak,3.the salt peak moving further downwards with the peak value decreasing.Results show that the maximum salt peak appears at the same depth if soil texture and outflow condition are the same.Factors affecting salt and water movement and ion components in the outflow solution underinfiltration are discussed.

Seasonal variability of salinity budget and water exchange in the northern Indian Ocean from HYCOM assimilation

Based on HYbrid Coordinate Ocean Model (HYCOM) assimilation and observations, we analyzed seasonal variability of the salinity budget in the southeastern Arabian Sea (AS) and the southern part of the Bay of Bengal (BOB), as well as water exchange between the two basins. Results show that fresh water flux cannot explain salinity changes in salinity budget of both regions. Oceanic advection decreases salinity in the southeastern AS during the winter monsoon season and increases salinity in the southern BOB during the summer monsoon season. In winter, the Northeast Monsoon Current (NMC) carries fresher water from the BOB westward into the southern AS; this westward advection is confined to 4°-6°N and the upper 180 m south of the Indian peninsula. Part of the less saline water then turns northward, decreasing salinity in the southeastern AS. In summer, the Southwest Monsoon Current (SMC) advects high-salinity water from the AS eastward into the BOB, increasing salinity along its path. This eastward advection of high-salinity water south of the India Peninsula extends southward to 2°N, and the layer becomes shallower than in winter. In addition to the monsoon current, the salinity difference between the two basins is important for salinity advection.

Does salinity change determine zooplankton variability in the saline Qarun Lake(Egypt)?

Zooplankton and 14 abiotic variables were studied during August 2011 at 10 stations in Lake Qarun, Egypt. Stations with the lowest salinity and highest nutrient concentrations and turbidity were close to the discharge of waters from the El-Bats and E1-Wadi drainage systems. A total of 15 holozooplankton species were identified. The salinity in Lake Qarun increased and fluctuated since 1901：12 g/L in 1901; 8.5 g/L in 1905; 12.0 g/L in 1922; 30.0 g/L in 1985; 38.7 g/L in 1994; 35.3 g/L in 2006, and 33.4 g/L in 2011. The mean concentration of nutrients （nitrate, nitrite and orthophosphate） gradually increased from 35, 0.16 and 0.38 μg/L, respectively, in 1953-1955 to 113, 16.4, and 30.26 μg/L in 2011. From 1999-2003 some decrease of species diversity occurred. Average total zooplankton density was 30 000 ind./m^3 in 1974-1977; 356 125 ind./m^3 in 1989; 534 000 ind./m^3 in 1994-1995; from 965 000 to 1 452 000 ind./m^3 in 2006, and 595 000 ind./m^3 in 2011. A range of long-term summer salinity variability during the last decades was very similar to a range of salinity spatial variability in summer 2011. There is no significant correlation between zooplankton abundance and salinity in spatial and long-term changes. We conclude that salinity fluctuations since at least 1955 did not directly drive the changes of composition and abundance of zooplankton in the lake. A marine community had formed in the lake, and it continues to change. One of the main drivers of this change is a regular introduction and a pressure of alien species on the existent community. Eutrophication also plays an important role. The introduction ofMnemiopsis leidyi, first reported in 2014, may lead to a start of a new stage of the biotic changes in Lake Qarun, when eutrophication and the population dynamics of this ctenophore will be main drivers of the ecosystem change.

Freshening of the intermediate water of the South China Sea between the 1960s and the 1980s

Variation in intermediate water salinity in the South China Sea (SCS) between the 1960s and 1980s was studied using historical hydrographic data. The results demonstrate that the water was significantly fresher in the 1980s than in the 1960s, indicating that vertical mixing at intermediate water depth was reduced in the 1980s. This was partially because of the change of the SCS meridional overturning circulation (MOC) connecting local intermediate water with deep water. Data assimilation showed a 0.5Sv (1 Sv=10 6m 3/s) reduction in the strength of the MOC, which is about one third of the mean SCS MOC. Because the SCS MOC is linked to the Pacific Ocean, such an interdecadal variation in the intermediate water SCS may reflect anthropogenic climate change in the world ocean.

Measurement and Correlation of Partition Coefficients of Baicalin in EOPO/Salt Aqueous Two-Phase Systems

The partition coefficients of baicalin were measured in ethylene oxide and propylene oxide (EOPO)/salt aqueous two-phase systems at 298.15K. It was found that most of baicalin partitioned into EOPO-rich phase. The partition coefficients of baicalin varied from 10 to 120. The effect of various factors, including tie-line length, salt composition, molecular weight of EOPO, and solution pH, on the partition behavior was investigated in EOPO/salt systems. Furthermore the partition coefficients of baicalin were correlated using the modified Diamond-Hsu model. Good agreement with experimental data is obtained. The average relative deviations are less than 5.0%.

Study on the treatment of eutrophic water with a new integrative apparatus for water purification

This paper studied the treatment of the landscape river in ChangZhou Scientific and Educational Town by a new integrative apparatus for water purification, which used ozone pre-oxidation-moDified clay-ozone biological activated carbon integrated process. The results indicate that the effectiveness of the algal removal with mentioned integrated process is much higher and the apparatus can operate stably. When the turbidity, chemical oxygen demand （CODMn）, total nitrogen （TN）, total phosphorus （TP） and algae densities of the raw water are 29-38 NTU, 7.45-7.79 mg/L, 2.496-2.981 mag/L, 0.237-0.255 mg/L and 5.78-7.94×10^8 cells/L respectively, it can be reduced to 0.8-1.7 NTU, 1.69-2.84 rag/L, 0.579-0.692mg/L, 0.013-0.038 mg/L, 0.06-0.38×10^8 cells/L. The average removal rates of turbidity, CODMn, TN, TP and algae density can reach 96.4%, 71.5%, 76.8%, 92.0% and 96.9% respectively. The treated water can meet the requirements of class Ⅰ- Ⅱ in Environmental Quality Standard, for Surface Water.