Spatial variation of phosphorus fractionation in the coral reef sediments of Lakshadweep Archipelago,Indian Ocean

Surface sediments were collected from the shore and lagoons of Kavaratti, Kadamat and Agatti islands of Lakshadweep Archipelago during May 2015 and analysed for the spatial distribution of the micronutrient element, phosphorus. Phosphorus was separated by sequential extraction procedure into five fractions – exchangeable (Ex-P), iron bound, (Fe-P), calcium bound (Ca-P), organic and residual fractions (OP) and total phosphorus (TP). The average relative contribution of each P species to TP was: OP?>?Ca –P?>?Ex – P?>?Fe – P. The high concentration of organic and residual phosphorus (87–96%) compared to inorganic phosphorus is particularly evident at stations characterised by higher total phosphorus concentrations. Among the three forms of IP in the sediments, Ca-P was dominant at all stations. The OC/OP ratio ranged from 3 to 163 in the sediments, suggesting that the organic matter in sediments had been subjected to degradation. Hence, the major contribution towards organic and residual phosphorus form is from the residual fraction comprising biologically resistant or non-available phosphorus form composed of refractory materials. The concentration of phosphorus reported in the present study is higher than that of the earlier studies in Lakshadweep, indicating a terrestrial and anthropogenic in?uence on the sediment.     

曝气复氧对富营养化水体底泥氮磷释放的影响

采用实验室模拟，研究了曝气复氧对富营养化水体底泥氮磷释放的影响，结果表明，①溶解氧是影响底泥氮磷释放的重要因素，厌氧状态会加速底泥氮磷的释放。②正常条件下曝气复氧可以有效的控制底泥总磷的释放；曝气条件下高pH值无法控制底泥总磷的释放，搅动会对底泥总磷的释放产生轻微的影响，上覆水总磷浓度较高时底泥会发生吸磷现象，而温度则影响较小。③正常条件下曝气复氧可以控制比较封闭水体底泥氨氮的释放；曝气条件下温度对底泥氨氮和总氮的释放影响较大，即温度越高，抑制氨氮和总氮的释放效果越好，且低温会导致底泥氨氮和总氮的大量释放；曝气条件下搅动导致底泥释放更多的氨氮和总氮。     

三峡水库香溪河库湾氮磷分布状况及沉积物污染评价

为了解三峡大坝蓄水完成之后香溪河库湾水体及沉积物中氮、磷的分布状况以及沉积物污染水平,2013年4月对三峡水库香溪河库湾进行调查采样,测定表层水及沉积物中氮磷含量和形态组成。结果表明,香溪河库湾表层水总磷(TP)含量范围为0.20~0.51 mg·L~(-1),总氮(TN)含量范围为0.54~2.25 mg·L~(-1),TP主要由磷酸盐(PO_4~(3-))组成,TN主要由硝酸盐(NO_3~-)以及氨氮(NH_4~+)组成,TP在空间上呈现从河口向库尾逐渐升高的分布格局,TN分布从河口向库尾逐渐降低。香溪河库湾沉积物中TP含量变化范围为642~1 189 mg·kg~(-1),TN含量变化范围为867~1 718 mg·kg~(-1),沉积物TP含量分布呈现上游高下游低,沉积物TN分布趋势呈现中间高,两头低。沉积物中TP主要由无机磷(IP)组成,有机磷(OP)所占比例较小,其中IP由钙磷(Ca-P)、铁铝磷(Fe/Al-P)组成,三者含量:Ca-POPFe/Al-P,且沉积物TP含量空间变化受到三者影响(P0.05)。采用单一因子标准指数法对香溪河库湾沉积物中TN、TP污染水平进行评价,结果表明,表层沉积物中TN、TP最低级别污染指数平均值为2.0和1.6,表层沉积物中TN、TP污染指数均超过最低污染水平,且TP的严重级别污染指数达到0.5以上。三峡水库三期蓄水完成以后,香溪河库湾表层水体中氮磷含量较初期蓄水有所升高,各样点沉积物中氮磷含量表现出相同的趋势,沉积物中不稳定磷释放对水体富营养化具有影响,香溪河库湾的表层沉积物已经受到一定的污染,磷污染水平较高。     

白洋淀沉积物中磷的存在形态及垂直变化规律研究

湖泊沉积物中磷的含量及其形态分布是影响湖泊营养化进程的极为重要因素,对研究湖泊营养化等环境问题具有重要意义。采用化学连续提取分析法,对白洋淀环淀中村水域不同地点的沉积物中磷的形态及其在垂直方向上的变化进行了研究。结果表明,研究区域内,环淀中村水域表层沉积物总磷（TP）质量分数在544.424～608.197mg·kg-1之间,无机磷（IP）是沉积物中磷的主要形态,有机磷（OP）质量分数较小,约占10%～27%,无机磷中钙磷（Ca-P）占的比例相对较大,在质量分数上约占75.8%～94.1%。从各形态磷质量分数的变化范围来看,Ca-P〉OP〉Fe/Al-P;人类活动对湖泊沉积物中磷的形态及其水平和垂向变化影响很大。     

Seasonal variation of nitrogen and phosphorus in Xiaojiang River—A tributary of the Three Gorges Reservoir

A yearlong monitoring program in the backwater area of Xiaojiang River (XBA) was launched in order to investigate the eutrophication of backwater areas in tributaries of the Yangtze River in the Three Gorges Reservoir (TGR) in China, starting after the impoundment water level of the TGR reached 156 m. From March 2007 to March 2008, the average concentration of total nitrogen (TN) and total phosphorus (TP) were (1553±484) μg·L^?1 and (62±31) μg·L^?1, respectively. The mean value of chlorophyll was (9.07±0.91) μg·L^?1. The trophic level of XBA was meso-eutrophic, while the general nutrient limitation was phosphorus. The results indicated that XBA has a strong ability to purify itself and has non-point source pollution from terrestrial runoff. The variation of TN/TP ratio was caused by a variation in TN rather than in TP when TN/TP < 22. N-fixation from cyanobacteria occurred and became an important process in overcoming the nitrogen deficit under a low TN/TP ratio. When TN/TP ? 22, the variation of TP affected the TN/TP ratio more significantly than TN. The increase of TP in XBA was caused mainly by particulate phosphorus, which could originate from a non-point source as adsorptive inorganic forms after heavy rainfall and surface runoff. An increase in the river’s flow could also contribute to an unstable environment for the growth of phytoplankton.     

Impacts of mussel dredging on sediment phosphorus dynamics in a eutrophic Danish fjord

Effects of mussel dredging on sediment metabolism (oxygen uptake and sulfate reduction rates) and phosphorus dynamics (flux across sediment-water interface and sequential extraction) were examined in Limfjorden (Denmark) during spring (May) and summer (August). Sediment samples were taken during mussel dredging and in addition an experimental simulation of the dredging was performed to investigate short-term changes in phosphorus (P) dynamics. Iron-bound P was reduced by up to 2/3 in the surface layer in the dredging track (from 31 to 8?mmol?P?m^?2), whereas the dissolved P-pools and less reactive particulate pools were not affected by dredging. Sediment oxygen consumption was enhanced immediately after dredging, but returned to the initial level after 4 days (20–40?mmol?m^?2?d^?1). The enhanced consumption was attributed to reoxidation of reduced compounds released during dredging. Sulfate reduction rates were high in the area (13–15?mmol?m^?2?d^?1) and sulfides competed with P for oxidized iron resulting in low iron-bound pools in the area (<4% of total P pools). Sulfate reduction rates were stimulated by the resuspension of sediments, especially in August, where a subsurface maximum was found, possibly due to a mixing of labile organic matter into these layers. In contrast sulfate reduction rates were reduced in the dredging track due to removal of labile organic matter from the surface layers. The loss of P during dredging was to some extent counteracted by regeneration of iron-bound P pools in the surface layers. The release of P due to mussel dredging was estimated to be in the same order of magnitude as the annual loading from the catchments and point sources to Limfjorden.     

黄河上中游表层沉积物磷的赋存形态特征

利用淡水沉积物中磷形态的标准测试程序（SMT）,研究了黄河上中游10个沉积物样品中磷的赋存形态变化规律和分布特征,并分析了沉积物中磷的来源和释放潜力。研究结果表明,黄河上中游沉积物中总磷（OP）的含量为82.0～113.5mg·kg-1,无机磷（IP）的含量范围在45.3～76.6mg·kg-1,有机磷（OP）的含量范围在27.6～56.6mg·kg-1。其中主要以无机磷的形式存在,而无机磷中以钙结合态磷为主。线性回归分析结果表明,NaOH-P的含量与活性态Fe、Al含量总和有一定的线性关系。黄河沉积物向上覆水体释放磷的潜力不大。     

Phosphorus speciation and effects of environmental factors on release of phosphorus from sediments obtained from Taihu Lake,Tien Lake,and East Lake

Phosphorus is considered the primary nutrient limiting eutrophication. The release of phosphorus from sediments not only provides hydrophytes with essential nutrients, but can also produce entrophication in lakes. In this study, the sediment characteristics, phosphorus speciation, and environmental factors affecting phosphorus release from sediments from Taihu Lake, Tien Lake, and East Lake were investigated. The results indicated that phosphorus levels of sediments ranged from 647 ± 67 to 2343 ± 122 mg/kg. Inorganic phosphorus comprised the majority of total phosphorus. The main phosphorus speciation of sediments obtained from Taihu Lake and Tien Lake was Residual-P, and the main phosphorus speciation of sediment obtained from East Lake was NaOH-P. Phosphorus release occurred in acidic and alkaline conditions but more frequently under alkaline conditions. The amount of phosphorus released from the sediments increased as the disturbing intensity rose. In addition, less phosphorus was released in natural than anaerobic conditions. The amount of phosphorus released was elevated as temperature increased.     

不同生态类型富营养化湖泊沉积物中有机质赋存形态

以藻型湖泊(太湖)、草藻型湖泊(南四湖)、草型湖泊(白洋淀)湖泊沉积物为研究对象,采集了11个表层沉积物样品,测定沉积物中总氮(TN)和总磷(TP)含量并利用物理分组方法,研究了3种不同生态型湖及同一湖泊不同区域沉积物中总有机质(OM)、轻组有机质(LFOM)和重组有机质(HFOM)的赋存特征.结果表明,南四湖沉积物中总氮、总磷和总有机质含量显著高于太湖和白洋淀;尽管太湖、南四湖和白洋淀沉积物中总有机质含量较高,但是轻组有机质(LFOM)含量较低,分别占总有机质的0.95%—1.08%、0.21%—1.37%和1.4%—1.78%;重组有机质(HFOM)含量较高,分别占总有机质的83.83%—87.4%、94%—98.98%和88.2%—98.3%,表明3种不同生态型湖泊沉积物中所含有机质绝大部分为难分解的重组有机质,轻组有机质基本矿化分解.相关性分析表明,轻组有机质(LFOM)、重组有机质(HFOM)与总有机质(OM)之间均呈现显著正相关关系.     

粤西三座重要供水水库沉积物营养盐负荷与重金属污染特征

为揭示粤西3座供水水库（高州水库、鹤地水库、大水桥水库）沉积物营养盐负荷及重金属污染特征,于2008年6月在各水库大坝前湖泊区采集柱状沉积物,运用SMT法、碱性过硫酸钾消解法、烧失法和ICP-MS法分别测定其柱状沉积物中氮磷营养盐、有机质和7种重金属（Cu、Pb、Zn、Cd、Ni、Cr与Hg）的含量,并采用潜在生态风险指数法对表层重金属污染的潜在生态风险进行评价,同时通过相关性分析重金属的可能来源。结果表明：3座水库沉积物总氮质量分数为1.13~3.37 mg·g-1,有机质为11.83~20.37 mg·g-1,其表层总氮、有机质的质量分数大小顺序为高州水库〉大水桥水库〉鹤地水库,总磷的质量浓度在0.22~0.77 mg·g-1之间,其表层总磷质量分数大小顺序为高州水库〉鹤地水库〉大水桥水库,在垂直剖面上,总氮、总磷与有机质的质量分数在16 cm至表层沉积物垂直断面显著高于其他断面,表明近些年来水库内源营养盐负荷逐渐加重。重金属质量分数平均值均高于广东省土壤环境背景值,总体呈现随深度增加而降低的趋势,但3座水库间重金属质量分数差异较大,其中鹤地和高州水库的Zn和Pb污染相对严重（质量分数分别为Zn：353.15、693.35 mg·kg-1;Pb：74.51、127.91 mg·kg-1）,大水桥水库的Cr和Ni污染相对严重（质量分数分别为Cr：238.69 mg·kg-1;Ni：251.06 mg·kg-1）。潜在生态风险评价表明,3座水库Cd和Hg具有高的生态危害,应引起重视,其他重金属则处于轻微的生态危害等级。同时沉积物高有机质的质量浓度经矿化分解可能加剧水体重金属生态危害。根据相关性分析和其他相关资料可知,粤西农业区大量化肥农药面源污染汇入造成水库初级生产力提高并最终沉降可能是沉积物营养盐、有机质与重金属的主要来源。     

南四湖沉积物营养盐释放特性

通过营养盐静态释放模拟试验,研究了南四湖沉积物NH4＋-N、TP和有机质（OM）的释放能力;针对微山湖区（WS）沉积物氮含量较高、释放较强的特点,为明晰WS湖区的氮释放潜力,考察了该湖区16个点位沉积物对NH4＋-N的等温吸附特性.静态释放试验表明,沉积物TP和OM释放能力较弱,对南四湖上覆水水质影响不明显;而WS湖区的NH4＋-N释放能力较强.WS湖区沉积物的NH4＋-N等温吸附试验表明,湖心区沉积物NH4＋-N释放能力最强,吸附/解吸平衡浓度（CEAC）高于1 mg.L-1的区域面积约占微山湖的1/5,该区域沉积物NH4＋-N释放将会对南水北调东线调水水质产生不利影响.     

微生物和硬毛藻对天鹅湖不同湖区沉积物氮磷释放的影响

荣成天鹅湖为一天然瀉湖,近年来绿潮硬毛藻大量爆发,内源污染日益严重。以大型硬毛藻和不同湖区沉积物为试材,设置沉积物+水、沉积物+水(灭菌)、沉积物+水+藻、沉积物+水+藻(灭菌)4个处理,研究了不同微生物活性及藻类条件下上覆水体氮磷质量浓度的变化,同步监测水土界面DO和pH等理化参数,以探讨藻分解和微生物对天鹅湖不同湖区沉积物氮磷释放的影响,为藻华消亡过程中内源污染的治理提供理论依据。结果表明,微生物存在和硬毛藻分解可使水体氮质量浓度明显增加(P<0.05)。试验过程中,水体总氮在有藻和无藻条件下的质量浓度变幅分别为1.56-14.11 mg·L^?1和0.11-8.96 mg·L^?1,后期灭菌处理明显低于未灭菌处理。藻分解对水体磷质量浓度具有极显著影响(P<0.01),有藻条件下灭菌处理总磷质量浓度为0.31-1.27 mg·L^?1,未灭菌处理为0.27-1.41 mg·L^?1;而无藻条件下灭菌和未灭菌处理变幅分别为0.019-0.047 mg·L^?1和0.025-0.078 mg·L^?1。在天鹅湖,不同湖区沉积物氮磷的释放能力存在差异,水体氮质量浓度在有藻和无藻条件下均表现为西北部>湖中心>湖南部,磷质量浓度有藻条件下与氮一致,而无藻条件下则表现为湖中心>西北部>湖南部。湖中心沉积物处理水体营养盐浓度受微生物活性影响较大。3种因素对水体氮磷质量浓度的影响效应表现为:藻类>微生物>沉积物。可见,在藻类大量暴发且微生物活性较高的湖中心及西北部,沉积物氮磷的释放潜力较大,尤其在藻类堆积腐烂时期,应引起足够重视。     

绿潮藻类暴发对天鹅湖水体和沉积物磷含量的影响

在荣成天鹅湖藻类暴发区域采集新鲜沉积物和丝状硬毛藻（Chaetomorpha spp.）,进行室内模拟试验,监测了生长过程中硬毛藻的生物量、磷富集量以及不同处理水体总磷（TP）和可溶性磷（SRP）质量浓度的变化,并分析了藻类生长对沉积物中各形态磷含量的影响。结果表明,当水体磷含量较高时,硬毛藻生长较快,相对生长速率高达14.88%,之后随着水体磷浓度的下降,生长速率逐渐减小。不同处理间硬毛藻的生物量相差很大,高磷含量处理显著高于低磷处理,最大差值可达26.50 g。随着藻类的生长,水体TP和SRP含量明显降低,其中高磷含量处理的TP质量浓度由0.93 mg·L-1降至0.01 mg·L-1,低磷含量处理水体SRP质量浓度均降至0.006 mg·L-1以下。当水体磷含量降至一定水平,沉积物中磷可向水体释放,其中可还原态磷和铁铝结合态磷的降幅分别为23.98%和12.61%。在高磷含量处理组,藻体中磷的富集量显著升高,且当水体磷含量相同的条件下,有沉积物处理的富集量显著高于无沉积物处理。相关分析表明,藻体生物量与水体TP和SRP的相关性较好,其中高磷含量处理组生物量与水体TP、SRP呈高度负相关,而相对生长速率与之呈显著正相关。结果说明,水体及沉积物中磷均可作为硬毛藻生长的营养来源;另一方面,藻类生长可明显降低水体磷含量,并促进沉积物中磷的释放。     

广东省不同水库底泥理化性质对内源氮磷释放影响

采用分级浸取分离方法,分析了广东省10个典型水库底泥的氮磷营养形态分布和污染状况;并通过模拟覆水试验,研究了不同水库底泥氮磷形态及理化性质对内源氮磷释放的影响。结果表明：广东省10个水库底泥氮磷污染较为严重,全氮含量为0.33~3.31 g.kg^-1,平均值为1.70 g.kg^-1;全磷含量为0.14~2.63 g.kg^-1,平均值为1.31 g.kg^-1。底泥氮磷主要以可转化态形式存在,可转化态氮磷含量占总氮磷含量百分比分别为41.2%~71.4%和53.6%~93.2%。底泥内源氮磷的释放主要受氮磷的赋存形态和含量的影响,水库底泥总氮的释放量与离子交换态氮（IEF-N）、碳酸盐结合态氮（WAEF-N）、铁锰氧化物结合态氮（SAEF-N）呈极显著正相关关系,相关系数分别为0.931、0.814、0.807;总磷的释放量与碳酸盐结合态磷（WAEF-P）、铁锰氧化物结合态磷（SAEF-P）呈极显著正相关,相关系数分别为0.960、0.957;这几种氮磷形态是上覆水体中氮磷的重要来源。同时底泥内源氮磷释放还与底泥机械组成有关,其中总氮和总磷释放量与底泥黏粒质量分数呈显著正相关,相关系数分别为0.738、0.638;而总氮的释放量与底泥砂粒质量分数呈显著负相关,相关系数为-0.685。这可能与可转化态氮磷更多的分布在细粒级底泥中有关,细颗粒底泥氮磷释放是上覆水体氮磷的主要来源。     

广州市流花湖表层底泥磷的形态与生物可利用性

应用经改进的Psenner连续提取法对广州市流花湖表层底泥中的磷进行了连续提取和测定。结果表明,流花湖底泥中总磷含量在1.28~2.15 mg/g,流花湖总磷含量最高在L2点,最低在L3点。湖泊表层底泥总磷主要由金属氧化物结合态磷、有机磷和钙结合态磷组成,可还原态磷和弱吸附态磷仅占很少部分。不同形态磷的含量顺序是金属氧化物结合态磷NaOH-P>有机磷Org-P>钙结合态磷HCl-P>可还原态磷BD-P>弱吸附态磷NH4Cl-P。底泥中生物可利用性磷的含量达0.76~1.00 mg/g,平均含量为0.91 mg/g,占总磷的45.47%~64.71%。说明流花湖底泥的磷有较好的生物可利用性,将为水体藻类大量繁殖提供潜在的有利条件,因此在湖泊治理恢复过程中,应该采样有效的措施来控制底泥磷的内源释放。     

菹草生长对沉积物间隙水中各形态磷浓度的影响

通过人工构建湖泊生态系统,用湖泊沉积物的上层泥和下层泥分别代表清淤前后的2种基质,研究菹草(Potamogeton crispus)生长对沉积物不同层次间隙水中各形态磷浓度的影响.垂直方向上,将2种基质中的间隙水分为表层、中层和底层3个层次.结果表明,菹草生长能够不同程度地降低各层间隙水中磷浓度,上层泥和下层泥2种基质均表现为表层间隙水溶解性总磷(DTP)和溶解性活性磷(SRP)含量降低幅度最大,DTP含量分别降低68.97％和83.09％,SRP含量分别降低54.57％和96.02％.菹草的吸收作用使得各层间隙水中磷浓度均低于无沉水植物的对照组.试验结束时,2种沉积物中TP含量降低幅度差异不显著,说明疏浚前后种植菹草均可有效控制湖泊内源磷污染.     

中国东部浅水湖泊沉积物总氮总磷基准阈值研究

受人类活动的影响,东部浅水湖泊沉积物中总氮、总磷负荷很高,当外来污染源得到控制时,底泥中的营养盐会逐渐释放出来,对湖泊水质与生态系统影响很大。为合理削减湖泊内源污染,控制沉积物中营养盐向上覆水体释放,研究制定东部浅水湖泊沉积物总氮、总磷基准阈值,分别测定了100个湖泊的896个表层沉积物样品和8个典型湖泊11个柱芯的沉积物总氮（TN）、总磷（TP）含量,分析了沉积物TN、TP浓度剖面分布特征。通过频度分布法对100个湖泊沉积物总氮总磷的污染状况进行评价,通过背景值比较法确定了8个典型湖泊沉积物的TN、TP背景值。结果表明,100个湖泊的表层沉积物TN浓度范围在479.70~5 573.65 mg·kg-1,TP浓度范围在248.44~1000.33 mg·kg-1,不同湖泊表层沉积物中TN、TP值差异较大。8个典型湖泊沉积物总氮、总磷含量整体上表现出随着深度增加而下降变化趋势,在深层沉积物中含量保持稳定。所调查8个湖泊TN均值为1443.83 mg·kg-1,变化范围为247.45~3719.46 mg·kg-1,各湖泊中TN均值表现为：沱湖〉焦岗湖〉花园湖〉七里湖〉北民湖〉大通湖〉城东湖〉瓦埠湖;TP均值为519.62 mg·kg-1,变化范围为225.41~1944.89 mg·kg-1,各湖泊中TP均值表现为：北民湖〉大通湖〉七里湖〉焦岗湖〉沱湖〉瓦埠湖〉城东湖〉花园湖。不同湖泊沉积物总氮、总磷背景值差异很大。通过对100个湖泊表层沉积物TN、TP的频度分析发现,沉积物营养盐含量上25%点位对应的TP质量浓度398.51mg·kg-1,TN质量浓度为1106.24 mg·kg-1,沉积物营养盐含量下25%点位对应的TP质量浓度664.58 mg·kg-1,TN质量浓度为2916.66 mg·kg-1。通过互相之间的比较分析,推荐采用背景值比较法确定的各湖泊沉积物总氮、总磷背景值均值与频度分步法25%点位对应的总氮值和40%点位对应的总磷值作为东部浅水湖泊沉积物总氮、总磷基准阈值。因此,?     

小流域土壤有机质和全磷空间变异分析——以安徽省舒城县龙潭小流域为例

为了解土壤的地域差异性,基于地统计学半方差函数理论和GIS空间克立格插值定量分析了安徽省舒城县龙潭小流域有机质、全磷的各向同性、各向异性变异特征及分布格局.结果表明,有机质、全磷的半方差拟合模型均为指数模型,两者的分布都显示了强烈的空间自相关,自相关距离分别为642 m、435 m.有机质、全磷变异的各向异性都比较显著,有机质在0°、50°方向上变异程度明显大于90°、145°方向;全磷则在0°、145°方向的变异程度更加突出.有机质、全磷的分布呈明显的块状和带状,其中有机质中部含量高,南部、西部含量低;全磷则是南部、西北含量高,西部、东北含量低.     

浮叶植物重建对富营养化湖泊氮磷营养水平的影响

利用太湖五里湖污染底泥，在不破坏表层沉积物形态和结构的情况下，利用大口径的采样器采集沉积物柱状样，研究浮叶植物荇菜（Limnanthemun nymphoides）在此底泥上适应性生长情况及其对水体以及沉积物中氮磷的影响。结果表明，在培养实验过程中，荇菜生长使上覆水体中的氮、磷营养水平逐渐降低，藻类的生长明显受到克制，水体透明度增加，水质逐渐改善。通过植物根系对沉积物和问隙水中营养盐的直接吸收，使表层（0～5cm）沉积物与问隙水中氮磷营养盐的水平在实验结束后有明皿下降，对于控制沉积物内源营养盐释放有重要的作用。因此，恢复以水生植物为丰的水生生态系统足重建富营养湖泊生态系统和控制湖泊内源负荷的重要措施。     

Phosphorus fractionation in surface water and sediments of industrially polluted freshwater reservoir,India

Industrial pollutions are responsible for alterations in biogeochemical cycling of phosphorus (P) in freshwater systems. The objectives of the present study were to quantify the major P forms and assess the relationship between P fractions in water and surface sediments of Govind Ballabh Pant Sagar (GBPS) reservoir, India. Surface water samples (n?=?48) and surface sediment samples (n?=?48) were collected from six regions of GBPS reservoir in December 2014. The results showed that total particulate phosphorus (TPP) and total dissolved phosphorus (TDP) account for 45%–58% and 42%–55% of total phosphorus (TP) in the surface water. The authigenic-P was found to be more than 84% of the total P in surface sediments. The TPP showed a positive statistical relationship with sedimentary P fractions (authigenic-P, exch-P, and organic-P) indicated the impact of industrial pollution load on inorganic and organic P fractions in water and sediments of GBPS reservoir. The discriminant fraction analysis (DFA) revealed that the exch-P, Fe(III)-bound-P, detrital-P, organic-P, and TPP were sensitive indicators of P dynamics in the industrially polluted GBPS reservoir.