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ICU hanging bridge is one of the essential salvage equipments in the guardian sickroom. It is consist of bridge, dry area and wet area. Its character lies in the logical separate structure between dry area and wet area.

ICU吊桥是现在重症监护病房必备的医疗抢救辅助设备，由桥架、干区和湿区组成，其特点在于合理的干湿分离结构。

Considering the difference of runoff characteristics on different underlying surface in the area of plain tidal river network, four kinds of surface is divided,namely, waters paddy field-, dry land and central urbanized area,and suitable method is adopted separately in each surface to simulate runoff process. Xinanjiang Model usually applicable for mountain areas is introduced to river network area, furthermore, the paper researches runoff calculation of central urbanized area, the underlying surface is divided into pervious and imperviousness areas.In perviousness areas, Hoton Infiltration formula and corresponding spatial infiltration rate curve are used to establish the relationship between infiltration rate and soil moisture in order to decide the infiltration. According to practical situation.

根据平原河网区城市下垫面产汇流方式的不同，分成水面、水田、旱地、城镇四类，分别采用相对应的产流汇流计算方法，将适用于山丘区的新安江模型引入到平原河网区城市，同时对于城镇这类下垫面，从下渗角度考虑，划分成透水和不透水两种类型，根据霍顿下渗公式和下渗率空间分布曲线，建立下渗率和土壤含水量的关系，进而研制出城镇透水面的产流计算方法，城镇汇流根据实际情况可结合城市管道排水计算。

The prediction results show that: by 2100, under the B1, the potential mire area will decrease about 54.16%, and mires will disappear in the south of the flat hilly regions and intermontane plains; under the SRES A1B, the potential mire area will decrease about 59.62%, and mires in south forest regions will disappear; under the SRES A2, the potential mire area will decrease about 73.51%, and mires will be found only in the north area with higher elevations.

所建模型具有很高的预测精度（ROC为0.96），预测结果表明：到2100年，SRES B1情景下，大兴安岭北部沼泽的潜在分布面积减少54.16%，南部相对平坦的丘陵和山间平原的沼泽大量消失；SRES A1B情景下，面积减少59.62%，南部林区的沼泽几乎全部消失；SRES A2情景下，面积减少73.51%，沼泽几乎完全退化到北部海拔较高处。

Xingtang County, Hebei Province, China Sun Life lithopone plant is the provincial advanced enterprise, founded in 1980, after more than two decades of construction, China has become a medium-sized inorganic chemicals, I plant located in the industrial area south of County Bank, an area of Area of 52,000 square meters, construction area of 14,600 square meters, fixed assets 12,000,000 yuan, with an annual output of 10,000 tons lithopone, the existing staff of 269, of whom 58 were technical staff.

河北省行唐县永明立德粉厂是省级先进企业，始建于1980年，经过二十多年的建设，已成为我国无机化工中型企业，我厂位于行唐县城南工业区，占地面积52000平方米，建筑面积14600平方米，固定资产1200万元，年产立德粉10000吨，现有员工269人，其中技术人员58人。我厂距石家庄飞机场35公里；距京广铁路新乐站和京深高速公路新乐出口14公里；紧邻朔黄铁路、张石高速公路，交通十分便利。

Based on GIS, the Akesu region was divided into four cotton planting zones: the premature long-staple cotton area, the premature and mid-mature land cotton area, the premature land cotton area and the extraordinary premature land cotton area.

近年来，气候以及棉花栽培技术都发生了变化，而地理信息技术的应用领域不断拓展，江西、陕西、安徽、山东等省气象部门相继开展了基于GIS的农业气候资源推算工作[1-8]，并在特色农产品区划等方面加以应用。

The site is the highly important mudflat area for many wildlife species and this sanctuary area has been recognized as a Protected Area by the International Union for Conservation of Nature and the United Nations Environment Programme and as an Important Bird Area by Bird Life International.

这里是很多野生动物物种栖息的重要滩涂，而且这一栖息地已被国际自然保护联盟和联合国环境规划署确认为保护区，并被鸟类生命国际确定为"重要鸟类栖息区"。

Some innovative results are listed below:1、According to the lithologic characters,lithofacies,genetic classification and the geomorphy,the Quaternary system is divided into piedmont-gully\'s and plain\'s. The piedmont-gully\'s Quaternary sediment,which is about 3～20 meters in thick,is in the western hills of the study area.The plain\'s Quaternary sediment is widely distributed in the study area,which is about 30～60meters thick and become thicker from southwest to northeast.2、The Quaternary sediments of plain can be divided into five sedimentary cycles.The Late Pleistocene series Quantan group,at the bottom of the Quaternary System,is constituted by a fluvial facies-river and lake facies sedimentary cycle. The Late Pleistocene series Jiashan group,at the middle of the Quaternary sediment, is constituted by two fluvial facies-neritic facies-river and lake facies sedimentary cycles.The Holocene series Binhai group,at the upper of the Quaternary sediment, is divided into three parts,the under layer and middle layer are constituted by two littoral facies-river and lake facies sedimentary cycles,the upper layer is constituted by paludal facies,which was deposited at the lower-lying land like West Lake, Jiangcun-Gu dang,Xianghu lake,and coastal-estuary facies in other area.3、Folding and fault activities were weak in Quaternary and the tectonic activity had little influence on the Quaternary sedimentation.The ancient landforms,the evolvement of the river system and transgression were the main elements which controlled the Quaternary sedimentation in Hangzhou.The ancient landforms formed the basis of the Quaternary sedimentation.The evolvement of the river system and transgression individually or jointly controlled the Quaternary sedimentation of this area.4、The alternation of the climate was the main reason for the evolvement of the river systems and transgression,and it\'s also the reason why the Quaternary system of Hangzhou has the special sedimentary structure which is called soft interbed with hard layers.

通过研究取得了以下成果：1、根据岩性、岩相、成因类型和地貌特点，将本区第四系划分为山麓沟谷区沉积和平原区沉积：山麓沟谷区第四系主要分布于西部丘陵地区，厚度较薄且变幅大，一般厚3～20m；平原区第四系广布分区，由南西向北东逐渐增厚，一般厚30～60m.2、平原区第四系自下而上大体由五个完整或不完整的沉积旋回构成：底部上更新统全塘组，由河流相—河湖相的沉积旋回构成；中部上更新统嘉善组，由河流相—浅海相—河湖相两个沉积旋回构成；上部全新统滨海组，其下中两段由滨海海湾相—河湖相的两个沉积旋回构成，上段由西湖、蒋村—古荡、湘湖等低洼处沉积的湖沼相和其他地区沉积的滨海河口相构成。3、第四纪以来，研究区内褶皱、断裂活动微弱，构造运动对第四系沉积的影响不大，古地形、古水系的发育、变迁和海侵是杭州市第四系沉积的主要控制因素：古地形构成了第四系沉积的基底，水系与海侵在其后的不同阶段或分别或联合的主导了区内的第四系沉积。4、水系的发育、变迁和海侵的共同原因是天气变化，正是由于第四纪以来"冷热交替"的天气特点形成了杭州市第四系"软硬互层"的特殊沉积结构。

The arable land area was increased a lot and garden plot area a little. The original pond was changed to the piscina. The graveyard area, the land area occupied by the use of farmland irrigation and road was reduced.

增加了大面积的耕地和少量的园地，将原有的坑塘水面部分整理成养殖水面，平掉原有的坟地，调整了农田水利用地和田间道路的占地面积，使之更为合理。

Comparing DW variation of area I~III with the north hemisphere tree rings, we also find that DW variation of these three areas are all good consistent with north hemisphere climate change; Comparing DW variation with pacific decadal oscillation and temperature variation of area I~III, we also find that WD variation of area I have good positive correlation with temperature variation; while the correlation of areas II and III is not better than that of area I.

此外，I~III区干湿变化的特征与北半球的气候变化有一定的对应关系；I区的干湿变化与当地的温度变化具有较好的正相关；II区和III区干湿变化与温度变化的联系相对I区差一些；太平洋年代际涛动可能对三个区域的干湿转化均有不同程度的影响。

The two preelection dredged-material Dump Sites (Mud Dump Site, area I and area II) is located in the area of the Yangxi sea area, about 7 and 9 km off the coast.

本研究在阳西海域划出两个预选倾倒区，对它们进行了水深和海流测量，通过数值模拟方式研究了该海域的流场、标识点的漂移路径和悬沙的迁移扩散，并探讨了疏浚物倾倒对海洋环境的影响。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。