[Kinetic Release Characteristics of Organic Phosphorus of Sediment-water and Water Quality Risks].

To reveal the characteristics of organic phosphorus release from lake sediments and its potential impact on water quality, six lake sediments from Yunnan Plateau and the middle and lower reaches of the Yangtze River in China were selected. We studied the differences in the kinetics of dissolved organic phosphorus (DOP) and dissolved inorganic phosphorus (SRP) release from sediments. The effects of organic phosphorus morphology and dissolved organic matter (DOM) characteristics on sediment phosphorus release were investigated, and the water quality risks of sediment DOP release were discussed. The results showed that:① the release kinetics of sediment DOP and SRP were similar; both followed the second-order kinetic model, starting with a rapid release phase, followed by a slow release, and the release curve gradually leveled off and reached the maximum release. ② The release of organic phosphorus was related to organophosphorus morphology and organic matter. Active organic phosphorus (LOP) and medium active organic phosphorus (MLOP) were the DOP forms mainly released into the overlying water during the rapid release phase. The proportion of LOP and MLOP to total organic phosphorus (DTP) decreased in the late release stage, whereas the proportion of non-active organic phosphorus (NLOP) increased; further, the degree of humification and aromaticity of organic matter gradually increased with phosphorus release, and its activity decreased, resulting in a slower release rate at the later stage. ③ Compared with that of SRP, the risk of DOP release was higher, accounting for 47%-77% of the total amount of DTP. It was also found that the higher the nutrient level of the lake, the greater the release of DOP and the higher the water quality risk. Therefore, not only the release of inorganic phosphorus but also that of organic phosphorus should be of concern in the process of phosphorus release from lake sediments to prevent the underestimation of phosphorus release and water quality risk.

[Spatio-Temporal Variation of Release Flux of Sediment Nitrogen and Phosphorus in High-Risk Period of Algal Bloom in Lake Erhai].

Spatial and temporal characteristics of release fluxes of sediment nitrogen (N) and phosphorus (P) were investigated in the high-risk period of algal blooms in Lake Erhai. Moreover, the influence factors were examined. Results show that the release flux of N and P increased in recent years, exhibiting a clear increase in the period from 2009 to 2013, and a slight increase in the period since 2013. The release flux of dissolved total nitrogen (DTN) ranged between 11.71-14.15 mg·(m2·d)-1, within which the release flux of dissolved organic nitrogen (DON) and dissolved inorganic nitrogen (DIN) were 6.39-8.42 mg·(m2·d)-1 and 5.31-5.73 mg·(m2·d)-1, accounting for 58% and 42% of the DTN, respectively. The release flux of dissolved total phosphorus (DTP) ranged between 0.11-0.14 mg·(m2·d)-1, within which the release flux of dissolved organic phosphorus (DOP) and dissolved inorganic phosphorus (DIP) were 0.04-0.05 mg·(m2·d)-1 and 0.07-0.09 mg·(m2·d)-1, accounting for 34% and 66% of the DTP, respectively. The distribution of release flux of N showed a decreasing order:south > north > middle, while P was north > middle > south. The release flux of N increased by 17%, 13% and 23%, and the release flux of P increased by 19%, 28%, and 29% in north, middle, and south part of Lake Erhai from 2009 to 2018. Comparing the years 2009, 2013 and 2018, although the contents of N and P were stable, the release flux of N and P in the sediment was enhanced due to increasing pH and decreasing DO. Therefore, the increasing release of nitrogen and phosphorus from sediments, caused by changes in the water environment factors, should be paid attention to for the protection of Lake Erhai.

[Correlation Analysis of Water Quality Between Lake Inflow and Outflow: A Case Study of Poyang Lake].

The relationships between inflow and outflow water quality data for Poyang Lake from 1996 to 2016 are discussed and the main influencing factors are identified. TN and TP were the main factors causing a decline in water quality in Poyang Lake during the study period. The water quality of both the inflow and outflow rivers was generally good between 1996 and 2003; however, water quality declined over the study period, which is attributed to an increase in nutrients loads in the watershed. From 2004 to 2011, the water quality of the "Five Rivers" decreased significantly, which caused the water quality of Poyang Lake to decline. Due to the high purification capacity of Poyang Lake, the water quality of the outflow during this period was relatively good. A decline in water quality after this point was affected by pollution loads and hydrological conditions. Specifically, from 2012 to 2016, water quality in Poyang Lake and of the inflow water declined further. This was combined with a decrease in the water-purification capacity of the lake due to changes in the hydrological conditions, resulting in lower water quality at the outflow. Overall, the water quality of the inflow river has been closely related to the water quality in Poyang Lake. The concentrations of TN were significantly higher in the southern and eastern areas of Poyang Lake compared to the western areas. Higher nutrient loading from the Ganjiang River and the Xinjiang River has been an important driver. The concentrations of TP in the southern area of the lake have been significantly higher than in the eastern and western areas. This is attributed to comparatively high TP loads in the Ganjiang River and the Fuhe River. Compared to the changes in hydrological conditions, variations in nutrient loading have had a greater effect on water quality in the lake.

[Effects and Differences of the Release of Dissolved Organic and Inorganic Phosphorus in Different Sediments Covered by Different Materials of Erhai Lake].

In this work, the effects of four covering materials on the release of total dissolved phosphorus (DTP), dissolved organic phosphorus (DOP), and soluble reactive P (SRP) in different sediments of Erhai Lake were simulated. The results showed that the max release of DTP was reduced in covering material, which attributed to the changes of pH, Eh and characteristics of dissolved organic matter (DOM) by the effect of covering material. The application of iron oxide material significant reduced the release of DTP in the northern and southern part of the lake, with decrease rate of 44.3% and 35.7%, respectively. by contrast, the application of aluminum oxide material significant reduced the release of DTP in the middle part sediment, with decrease rate of 29.6%. Furthermore, the release of SRP and DOP in different sediments has significant difference after added different material. In northern part of sediment, the release of SRP and DOP reduced by 35.6% and 36.2% after added iron oxide material. This is because iron oxide can reduce the pH and Eh but increase the availability of DOM in northern, and then benefits for inhibiting the release of SRP and DOP. In the middle, the release of sediment SRP and DOP reduced by 28.9% and 31.6% after added aluminum oxide material. This is because the aluminum oxide can facilitate the availability of DOM in middle, and then inhibits the release of SRP and DOP. In southern part of the lake, the release of sediment SRP and DOP reduced by 47.4% and 16.5% after added iron oxide material. This is largely attributed to the effect of iron oxide on the pH and Eh. Therefore, to control the release of P in the sediment from Lake Erhai, iron oxide material should be selected in the northern and southern parts, whereas aluminum oxide should be selected in the middle part of the lake.

[Distribution of transferable nitrogen in Poyang Lake sediments and its response to the variation of River-Lake relationship].

Amounts and distributions of total transferable nitrogen and different transferable nitrogen forms were studied in the sediments of Poyang Lake with different regimen, in order to reveal the influence of the water level change caused by the River-Lake relationship change on the potential release risks of nitrogen. The results showed that: (1) the contents of the total nitrogen (TN) were between 389 and 3865 mg x kg(-1), and the spatial distribution showed an overall downward trend in the "Five River", the "Hu Xin" and the northern regions; the contents of the transferable total nitrogen (TTN) were between 319.36 and 904.56 mg x kg(-1) and contributed 52% to the TN, and its spatial distribution trend was the same as that of TN. (2) The content of transferable nitrogen followed the order of SOEF-N approximately = SAEF-N > WAEF-N > IEF-N. (3) The dry period advanced and the low water level continued to decline as a result of the change in River-Lake relationship of the Poyang Lake, leading to the prolonged outcropped time of sediments and the increased area, causing the different contents of transferable nitrogen in the sediments at different elevations. The transferable nitrogen content of the sediments in the whole lake during the wet period was lower than that during the dry period. The content of transferable nitrogen followed the order of 12-13 m elevation sediment > 11-12 m elevation deposition material > 10-11 m elevation sediments. The higher the elevation, the longer the sediments were exposed, and the higher the transferable nitrogen content. (4) With the increase of elevation, all forms of N contents increased. The increase of IEF-N and SOEF-N contents as well as their percentages in total transferable nitrogen was relatively small, while the increase of WAEF-N and SAEF-N contents as well as their percentages in total transferable nitrogen was relatively large. If the river-lake relationship changes further, the elevation in the dry period will further decrease, which will lead to the enlarged area and prolonged exposure of sediments, resulting in increase of TN, transferable nitrogen, IEF-N and SOEF-N contents in the sediments. At the coming wet period of next year, the nitrogen release risk from sediments of Poyang Lake might increase.

[Influence of the river-lake relation change on the distribution of heavy metal and ecological risk assessment in the surface sediment of Poyang Lake].

Effects of river (Yangtze River)-lake (Poyang Lake) relation on the distribution and potential ecological risk of Cu, Pb, Zn, Cr and Cd were investigated in surface sediment of Poyang Lake under different waterregimens. The results indicated: (1) the sediments of Poyang Lake were polluted by various concentrations of heavy metals mainly originated from particulates of Yangtze River, and Cu and Pb were the main pollution factors. The pollution level of determined heavy metals followed the order of Cu > Pb > Zn > Cr >Cd. The concentration ranges of Cu, Pb, Zn, Cr and Cd in the sediment of Poyang Lake were 13.1-108.1 mg.kg-1 , 37-119.1 mg.kg-1, 29.9-129.9 mgkg-1, 13.3-98.6 mgkg-1 and 0. 19-2.77 mg.kg-1 during the wet period, and 3.05-69.7 mg.kg-1, 27.5-105 mgkg-1, 18.8-95.4 mg.kg-1, 7.34-70 mg.kg- and 0.033-0.406 mg.kg-1 during the dry period respectively. The region with the highest heavy metal concentrations was located in water input area of the " Five River" and water output area of " Hukou" ; (2)The regions with high risk of heavy metals in sediment were mainly located in the area of the trail of "Five Rivers" during the wet period; while during the dry period, the area with high risk of heavy metals in sediment enlarged, which was not only limited in the area of the trail of "Five Rivers", but also enlarged northwards. The potential ecological risk of "Hukou" was relatively high, however, the potential ecological risk of the sediment in the whole lake during the dry period was lower than that during the wet period. (3) With the change of river-lake relation, water level rose, the maintaining time was shortened during the wet period, the dry season appeared ahead of schedule, the transformation course of Poyang Lake from "Lake morphology" to " River morphology" increased, and the typical river properties were enhanced, which resulted in the decreased potential ecological risk of heavy metals in sediment of the whole lake, however, the area of high risk-region was enlarged northwards.