Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, PR China.
Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, PR China; Function laboratory for Marine Ecology and Environmental Science, Qingdao National Oceanography Laboratory, Qingdao 266100, PR China.
Sci Total Environ. 2017 Aug 15;592:161-170. doi: 10.1016/j.scitotenv.2017.03.098. Epub 2017 Mar 29.
Anthropogenic activities alter the natural states of large rivers and their surrounding environment. The Yellow River is a well-studied case of a large river with heavy human control. An artificial managed water and sediment release system, known as the Water-Sediment Regulation Scheme (WSRS), has been carried out annually in the Yellow River since 2002. Nutrient concentrations and composition display significant time and space variations during the WSRS period. To figure out the anthropogenic impact of nutrient changes and transport in the Yellow River, biogeochemical observations were carried out in both middle reaches and lower reaches of the Yellow River during 2014 WSRS period. WSRS has a direct impact on water oxidation-reduction environment in the middle reaches; concentrations of nitrite (NO) and ammonium (NH) increased, while nitrate (NO) concentration decreased by enhanced denitrification. WSRS changed transport of water and sediment; dissolved silicate (DSi) in the middle reaches was directly controlled by sediments release during the WSRS while in the lower reaches, DSi changed with both sediments and water released from middle reaches. During the WSRS, the differences of nutrient fluxes and concentrations between lower reaches and middle reaches were significant; dissolved inorganic phosphorous (DIP) and dissolved inorganic nitrogen (DIN) were higher in low reaches because of anthropogenic inputs. Human intervention, especially WSRS, can apparently change the natural states of both the mainstream and estuarine environments of the Yellow River within a short time.
人为活动改变了大河及其周围环境的自然状态。黄河是受人类控制严重的大河的典型案例。自 2002 年以来,黄河每年都实施一项名为“水沙调控”的人工调水调沙工程。在调水调沙期间,养分浓度和组成表现出显著的时间和空间变化。为了了解黄河养分变化和输移的人为影响,2014 年调水调沙期间在黄河中游和下游进行了生物地球化学观测。调水调沙直接影响了黄河中游的氧化还原环境;由于反硝化作用增强,亚硝酸盐(NO)和铵(NH)浓度增加,而硝酸盐(NO)浓度降低。调水调沙改变了水沙输移;黄河中游的溶解硅酸(DSi)直接受调水调沙期间泥沙释放的控制,而在下游,DSi 随中游来水和泥沙共同变化。调水调沙期间,下游和中游的养分通量和浓度差异显著;由于人为输入,下游的溶解无机磷(DIP)和溶解无机氮(DIN)较高。人类干预,特别是调水调沙,可以在短时间内明显改变黄河干流和河口环境的自然状态。