Response of Water Cycle Processes in Sanjiang Plain to Human Activities and Climate Change in Recent 50 Years

Chen Zhi-ke
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引用次数: 4

Abstract

Impacts of human activities on water cycle process in Sanjiang plain mainly include:①large-scale hydro-junction project dramatically weakened the flood processes of Heilongjiang,Wusuli and Songhua Rivers flowing through Sanjiang plain sections,and reduced natural groundwater and surface water recharges opportunities and amount for Sanjiang plain;②construction of large number of drainage canals enhanced the hydrological gradient of regional drainage,and accelerated the generation and distribution processes of surface runoff;③conversion from glebe into paddy field enhanced the utilization efficiency of effective precipitation,reduced the regional surface runoff depth,and enlarged the regional evapotranspiration;④area enlargement of well-irrigated rice field drives large-scale groundwater exploitation,which leads to the imbalance of exploitation and recharge of groundwater,the continuous decline of the groundwater table,and the reduction of groundwater storage volume;⑤deforestation in the headstream region,which causes the reduction of the proportion of snowfall converting into surface runoff and the decline of water conservation capabilities of forest soil.The resulting influences human activities have on water cycle processes in Sanjiang plain are that water input is decreasing and water output is increasing.Major impacts from climate change on water cycle process mainly include:①total area precipitation shows a declining trend,but not obvious;②regional temperature and potential evaporation are rising;③the rise of land temperature is the most obvious,the permafrost layer is becoming thinner,duration of permafrost fusion is shortened by 55 to 62 days,and the soil moisture of permafrost layer is apparently lower than that 50 years ago.Cultivated soil water moisture visibly declines.These changes will not benefit the surface runoff generation and precipitation infiltration to recharge groundwater,Based on the water cycle processes analysis,it is concluded that Sanjiang plain is getting drought.Therefore,strengthening the development and application of agricultural conservation tillage measures,as well as speeding up the restoration of degraded wetland water resources,enhancing the regional water storage capacity and water saving level in agricultural aspect will be important directions to ensure Sanjiang plain water security.
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近50年来三江平原水循环过程对人类活动和气候变化的响应
人类活动对三江平原水循环过程的影响主要表现在:①大型水利枢纽工程显著削弱了流经三江平原的黑龙江、乌苏里江和松花江的洪水过程,减少了三江平原天然地下水和地表水的补给机会和补给量;②大量排水渠的建设增强了区域流域的水文梯度,加速了水循环的产生和分布③地表径流向水田的转化提高了有效降水的利用效率,降低了区域地表径流深度,增大了区域蒸散量;④井灌水田面积的扩大带动了地下水的大规模开采,导致地下水开采与补给不平衡,地下水位持续下降,地下水库存量减少源区,导致降雪转化为地表径流的比例降低,森林土壤保水能力下降。人类活动对三江平原水循环过程的影响表现为水输入减少,水输出增加。气候变化对水循环过程的影响主要表现为:①总降水量呈下降趋势,但不明显;②区域温度和潜在蒸发量呈上升趋势;③地表温度上升最为明显,多年冻土层变薄,多年冻土层融合时间缩短55 ~ 62 d,多年冻土层土壤水分明显低于50年前。耕地土壤水分明显下降。这些变化不利于地表径流的生成和降水入渗补给地下水,通过对水循环过程的分析,认为三江平原正处于干旱期。因此,加强农业保护性耕作措施的开发和应用,加快退化湿地水资源的恢复,提高区域蓄水能力和农业节水水平,将是保障三江平原水安全的重要方向。
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期刊介绍: "South-to-North Water Transfers and Water Science and Technology" was founded in 2003, mainly publishing papers on water science, water engineering, water resources, water environment, water management, etc. The journal currently has the following columns: hydrology and water resources, ecology and environment, high-quality development of follow-up projects of South-to-North Water Transfers and construction of national water network, ecological protection and high-quality development of the Yellow River Basin, flood disasters and response, "dual carbon" and water conservancy technology, efficient utilization of agricultural water and soil resources, hydrogeology and engineering geology, etc. The journal is now a Chinese core journal; a source journal for Chinese scientific and technological papers (Chinese core journals); a source journal for the Chinese Science Citation Database (CSCD); and a Chinese core academic journal (A) of RCCSE.
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