Abstract:As part of a study using lake sediments to determine the extent and causes of human impacts to lakes along an east-west transect following the Yangtse River, sediment cores were taken from Taihu in eastern China. Previous studies have focussed on the impacts of direct inputs of pollutants from municipal and industrial wastewater but little work has been undertaken on trends in atmospheric deposition from the many industrial sources surrounding the lake. Analysis of the Taihu sediment cores for atmospheric poll… Show more
“…8). The extent of the Pb enrichment at the CH1 site was comparable to many lakes located in the middle and Yangtze River Basin in which there is no point pollution of Pb (Rose et al, 2004;Liu et al, 2007;Yao et al, 2009;Yuan et al, 2011). The low enrichment of Pb at CH1 implies that the atmospheric source of Pb loading to the lake cannot be ignored or may even be a major source to the lake sediment at the CH1 site.…”
Section: Sources Of Anthropogenic Heavy Metalmentioning
confidence: 72%
“…According to a simple surface sediment survey conducted by the Nanjing Institute of Geography and Limnology of the Chinese Academy of Sciences in 2007, the Cu content ranged from 36.3-382.3 mg kg Paleolimnology offers a unique historical perspective for the study of the effects of the Wushan Copper Mine activities on Chihu Lake and the pre-disturbance environmental conditions of the lake. An analysis of the trace metals in the lake sediment cores with the chronology can provide valuable insights into the historical metal inputs (Boyle et al, 1999;Rose et al, 2004;Yang and Rose, 2005;Couillard et al, 2008). Heavy metals in the Chihu Lake sediments include not only the anthropogenic source but also the metal from the natural input of the catchment.…”
Section: Introductionmentioning
confidence: 99%
“…Using the CIC (constant initial concentration) model of 210 Pb, the average sediment rate of 0.84 cm a -1 can be calculated in the section in the CH1 core, which was quite different from 137 Cs result. 210 Pb CRS (constant rate of supply of 210 Pb ) model and composite model from CRS are commonly used to date sediment ages of shallow lakes at Yangtze River Basin (Rose et al, 2004;Wu et al, 2008;Liu et al, 2012;Yao and Xue, 2015). The CRS model Pb and the sediment depth in the CH2 core.…”
Two short sedimentary cores were collected in 2012 from Chihu Lake in the middle Yangtze River Basin using a gravity corer. Heavy metals, including Pb, Cu, Zn, Cd, Cr, Co, Ni and Mn, and major elements, including Al, Fe, K, Mg and Ti, were
“…8). The extent of the Pb enrichment at the CH1 site was comparable to many lakes located in the middle and Yangtze River Basin in which there is no point pollution of Pb (Rose et al, 2004;Liu et al, 2007;Yao et al, 2009;Yuan et al, 2011). The low enrichment of Pb at CH1 implies that the atmospheric source of Pb loading to the lake cannot be ignored or may even be a major source to the lake sediment at the CH1 site.…”
Section: Sources Of Anthropogenic Heavy Metalmentioning
confidence: 72%
“…According to a simple surface sediment survey conducted by the Nanjing Institute of Geography and Limnology of the Chinese Academy of Sciences in 2007, the Cu content ranged from 36.3-382.3 mg kg Paleolimnology offers a unique historical perspective for the study of the effects of the Wushan Copper Mine activities on Chihu Lake and the pre-disturbance environmental conditions of the lake. An analysis of the trace metals in the lake sediment cores with the chronology can provide valuable insights into the historical metal inputs (Boyle et al, 1999;Rose et al, 2004;Yang and Rose, 2005;Couillard et al, 2008). Heavy metals in the Chihu Lake sediments include not only the anthropogenic source but also the metal from the natural input of the catchment.…”
Section: Introductionmentioning
confidence: 99%
“…Using the CIC (constant initial concentration) model of 210 Pb, the average sediment rate of 0.84 cm a -1 can be calculated in the section in the CH1 core, which was quite different from 137 Cs result. 210 Pb CRS (constant rate of supply of 210 Pb ) model and composite model from CRS are commonly used to date sediment ages of shallow lakes at Yangtze River Basin (Rose et al, 2004;Wu et al, 2008;Liu et al, 2012;Yao and Xue, 2015). The CRS model Pb and the sediment depth in the CH2 core.…”
Two short sedimentary cores were collected in 2012 from Chihu Lake in the middle Yangtze River Basin using a gravity corer. Heavy metals, including Pb, Cu, Zn, Cd, Cr, Co, Ni and Mn, and major elements, including Al, Fe, K, Mg and Ti, were
“…For ex am ple, the contents of sil ica, po tas sium and alu mi num are com monly con sidered as in di ca tors of me chan i cal de nu da tion in ten sity, whereas the con tent of cal cium re flects the in ten sity of chem i cal de nu dation. The abun dance of ni tro gen and phos pho rus pro vides in forma tion about trophic con di tions; con cen tra tions of heavy metals are in di ces of hu man ac tiv ity (Ham il ton-Tay lor, 1979;Abraham, 1998;Last and Smol, 2001;Rose et al, 2004;Jin et al, 2006;Borówka, 2007;Schmidt et al, 2008;Paw³owski et al, 2015a, b). How ever, pri mary fea tures of sed i ments can undergo trans for ma tion in post-sed i men ta tion pro cesses (Boyle, 2001;Hag gard et al, 2005;Wil son et al, 2008), which may ham per cor rect in ter pre ta tion.…”
Late Pleis to cene and Ho lo cene en vi ron men tal evo lu tion of the Wkra River Val ley near Bielawy Go³uskie (cen tral Po land) re corded in palaeo-ox bow lake de pos its Monika This study aimed to re con struct en vi ron men tal changes in the Wkra River Val ley near Bielawy Go³uskie (cen tral Po land) based on geo chem i cal, palynological and subfossil Cladocera anal y sis of de pos its fill ing a palaeo-ox bow lake. Two sed iment bore holes col lected from the palaeochannel bend (BG-1) and neck (BG-2) in clude full se quences of or ganic de pos its ly ing on clastic de pos its. The lower part of the BG-1 bore hole con tains gyttja that ac cu mu lated dur ing the Youn ger Dryas and the Preboreal, which is cov ered by reed peat of Preboreal and Bo real age. On top of this is al der peat that ac cu mu lated during the At lan tic. The ages of the gyttja and peat were con firmed by both ra dio car bon dat ing and palynological anal y sis. The peats are char ac ter ized by a sig nif i cant con tent of or ganic mat ter, which is rel a tively sta ble over time. This in di cates a low inten sity of me chan i cal de nu da tion in the catch ment, which is sup ported by low con cen tra tions of alu mi num and po tas sium. Cal cium val ues greatly ex ceed these el e ments, sug gest ing that the lake was mainly fed by ground wa ter. Vari a tion in trophic con di tions over time is in di cated by a ver ti cal vari abil ity in the con tent of ni tro gen, as well as by the Cladocera pop u la tion. The strong de com po si tion of peat in the top layer of the mire, and in creased con cen tra tions of phos pho rus and heavy met als, testify to in creas ing hu man ac tiv ity dur ing the most re cent time pe ri ods.
“…Urban watersheds generally produce higher unit area nutrient loadings from runoff and sewage, compared to other watersheds (Naselli-Flores, 2008). In addition, industrial activities produce large amount of metals that are easily transported to urban lakes by water runoff (Boyle et al, 1999;Rose et al, 2004;Wu et al, 2012). Thus, urban lakes collect and accumulate large amount of nutrients and metals.…”
-Diatoms and geochemical stratigraphy were studied in sediment core samples collected from a heavily polluted urban lake (SE China) in order to track the history of eutrophication and heavy metal contamination. The sediment profile covered ca. 60 years (from ca. 1951 to 2011) based on 137 Cs and Spheroidal carbonaceous particles (SCP) dating, and encompassed a period of rapid industrial development in this region. Diatoms experienced two visible shifts, including the replacement of benthic and epiphytic taxa by planktonic species (e.g., Cyclotella meneghiniana Ku¨tzing) in 1972, and the dominance of Cyclotella atomus Hustedt and Nitzschia palea (Ku¨tzing) W. Smith after 1999. Metals (i.e., Cd, Pb and Zn), total phosphorus, total nitrogen and total organic carbon all increased in the past 60 years. Redundancy analysis was used to correlate diatom with chemical change and explained 50.3-60% of total variation in diatom data for three periods (from 1951 to 1999, between 1951 and 2011 and from 1972 to 2011). The combined effects of nutrients and metals were the predominant factor, capturing 29.6-42.8% of the total variance. Nutrients alone accounted for little more variance than did metals alone for the first flora shift about 1972. The further shift after 1999 was more influenced by the sole effect of metals than that of nutrients. Increases in species (e.g., N. Palea) able to tolerate both nutrient-related and metal-related stressors were related to persistent nutrient and metal inputs. In addition, climate warming might exacerbate eutrophication and metal contamination in this lake.
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