徐福顺副省长对国土资源工作提出五点要求

<正>11月2日上午,徐福顺副省长在听取刘山青厅长关于近期国土资源工作情况汇报后指出,今年以来,省国土资源厅党委班子紧紧围绕"四个发展"要求,以"358"地勘     

张光荣副省长在青海东部黄河谷地百万亩土地开展整理重大项目开工典礼上的致辞（2010年10月9日）

10月9日,秋高气爽,风和日丽。化隆回族自治县甘都镇隆康村红山根下,彩旗招展,人头攒动,随着省委副书记、省长骆惠宁宣布青海东部黄河谷地百万亩土地开发整理重大项目正式开工,礼炮齐鸣,焰火缤纷,群山为之欢笑,大地为之共鸣。至此,年增产粮食2．5亿斤;年增木材蓄积量30万立方米;年增产总值4．12亿元;可容纳安置近15万人……随着青海东部黄河谷地百万亩土地开发整理重大项目的启动,从“九曲黄河引上山,旱台变成米粮川”的期待到“田成方、渠相连、路相通、林成网”的农业新格局的实现,不再是一个梦想,古老的黄河谷地将孕育更新更多的希望。     

加快推进百万亩重大项目

<正>9月14日下午,省委常委、常务副省长,青海东部黄河谷地百万亩土地开发整理重大项目领导小组组长徐福顺主持召开领导小组第一次会议,安排部署百万亩重大项目工程实施相关工作。省百万亩重大     

秉公执法 不负民望

从2009年开始,焦作市着手对辖区内的黄河滩涂进行生态开发。一年来,已开发高效农业生态园区6万余亩,其中,新增耕地54942．6亩。     

山东黄河冲积平原区地氟病与地球化学环境相关性研究

山东黄河冲积平原区是山东省地氟病的重病区,危害严重。选择其中的郓城、嘉祥、博兴3县进行土壤氟含量、饮水氟含量、儿童尿氟、儿童氟斑牙检出率、氟斑牙指数、成人尿氟、成人氟骨症检出率等指标进行调查,结果表明区内土壤、饮水氟含量和群体的尿氟含量普遍较高,高氟的危害和地方性氟中毒病情十分严重。在分析氟元素在土壤、饮水中的分布及变化规律的基础上,开展地方性氟中毒病与生态地球化学环境相关性研究,认为地方性氟中毒病与土壤中氟含量、饮水氟含量呈正相关关系。     

2008年黄河入海口潮间带大型底栖动物生物量研究

于2008年5月(枯水期)和8月(丰水期),分别对黄河入海口潮间带大型底栖动物进行了野外调查与研究。结果表明,底栖动物生物量平均为177.23±55.56 g.m-2,软体动物占据绝对优势;各潮带丰水期底栖动物生物量较枯水期增加,且低潮带>中潮带>高潮带。底栖动物栖息密度平均为573.07±125.60 m-2,软体动物栖占据绝对优势,丰水期底栖动物栖息密度较枯水期升高。四角蛤蜊(Mactra veneriformis)、泥螺(Bullacta exarata)、双齿围沙蚕(Perinereis aibuhitensis)、彩虹明樱蛤(Moerella iridescens)、天津厚蟹(Helice tientsinensis)、青蛤(Cyclina sinensis)、豆形拳蟹(Philyra pisum)、光滑河蓝蛤(Potamocorbula laevis)、托氏昌螺(Umbonium thomasi)和短文蛤(Meretrix pethechialis)等种类的相对重要性指数值较高。     

近60年黄河水沙变化及其对三角洲沉积的影响

In order to find out the variation process of water-sediment and its effect on the Yellow River Delta, the water discharge and sediment load at Lijin from 1950 to 2007 and the decrease of water discharge and sediment load in the Yellow River Basin caused by human disturbances were analyzed by means of statistics. It was shown that the water discharge and sediment load into the sea were decreasing from 1950 to 2007 with serious fluctuation. The human activities were the main cause for decrease of water discharge and sediment load into the sea. From 1950 to 2005, the average annual reduction of water discharge and sediment load by means of water-soil conservation practices were 2.02×109 m3 and 3.41×108 t respectively, and the average annual volume by water abstraction for industry and agriculture were 2.52×1010 m3 and 2.42×108 t respectively. The average sediment trapped by Sanmenxia Reservoir was 1.45×108 t from 1960 to 2007, and the average sediment retention of Xiaolangdi Reservoir was 2.398×108 t from 1997 to 2007. Compared to the data records at Huanyuankou, the water discharge and sediment load into the sea decreased with siltation in the lower reaches and increased with scouring in the lower reaches. The coastline near river mouth extended and the delta area increased when the ratio of accumulative sediment load and accumulative water discharge into the sea (SSCT) is 25.4–26.0 kg/m3 in different time periods. However, the sharp decrease of water discharge and sediment load into the sea in recent years, especially the Yellow River into the sea at Qing 8, the entire Yellow River Delta has turned into erosion from siltation, and the time for a reversal of the state was about 1997.     

黄河入海悬沙季节输送变化与输送机制的数值研究(英文)

Based on sediment and discharge flux data for the Yellow River, realistic forcing fields and bathymetry of the Bohai Sea, a suspended sediment transport module is driven by a wave-current coupled model to research seasonal variations and mechanisms of suspended load transport to the Bohai Sea. It could be concluded that surface sediment concentration indicates a distinct spatial distribution characteristic that varies seasonally in the Bohai Sea. Sediment concentration is rather high near the Yellow River estuary, seasonal variations of which are controlled by quantity of sediment from the Yellow River, suspended sediment concentration reaches its maximum during summer and fall. Furthermore, sediment concentration decreases rapidly in other seas far from the Yellow River estuary and maintains a very low level in the center of the Bohai Sea, and is dominated by seasonal variations of climatology wind field in the Bohai Sea. Only a small amount of sediments imported from the Yellow River are delivered northwestward to the southern coast of the Bohai Bay. Majority of sediments are transported southeastward to the Laizhou Bay, where sediments are continuously delivered into the center of the Bohai Sea in a northeastward direction, and part of them are transported eastward alongshore through the Bohai Strait. 69% of sediments from the Yellow River are deposited near the river delta, 31% conveyed seaward, within which, 4% exported to the northern Yellow Sea through the Bohai Strait. Wind wave is the most essential contributor to seasonal variations of sediment concentration in the Bohai Sea, and the contribution of tidal currents is also significant in shallow waters when wind speed is low.     

寻找“木根山”

<正>公元365年和392年,前秦帝国的氐族皇帝苻坚与北魏王朝的开国君主拓跋珪,都曾进入鄂尔多斯地区巡游。他们之所以对这片土地发生兴趣,都与制服这里的铁弗匈奴有关,也都涉及到古河套中一个神秘的地名——木根山。     

人水和谐相处——不与水争地

<正>我国古代,有一位治水名人,他就是西汉后期的贾让。贾让通过对黄河河道变迁的历史分析,指出黄河泛滥的根源是人们过度占据了河流的容水之地。治河应当给河流