四川农业大学自然地理学(本科)1

奥鹏四川农业大学在线考核满分答案参考

{"P1":"e69ca720-8933-4d04-9ff5-ab60de8ea906","P2":"自然地理学(本科)-00001","data":[{"I1":"17de8582-7550-4d32-ae08-7c95c56bf520","I2":["综合自然地理环境各组成要素中，（ ）是大陆纬度地带性最明显的标志。"],"I3":1,"I6":["气候","地貌","植被","土壤"],"I15":["2"]},{"I1":"41bda831-27c6-472c-a7f9-6d1ad097186d","I2":["南半球缺乏的植被类型有（ ）。"],"I3":1,"I6":["夏绿阔叶林","热带季雨林","寒温性针叶林","热带雨林"],"I15":["2"]},{"I1":"038b91f6-2316-4667-94f1-d99ed35a1f35","I2":["下列矿物中，（ ）是岩浆岩中SiO2过饱和的指示矿物。"],"I3":1,"I6":["长石","石英","辉石","镁橄榄石"],"I15":["1"]},{"I1":"37ca987b-40e4-43ea-843a-7ebede067e26","I2":["不属于地表水的补给方式是（ ）。"],"I3":1,"I6":["雨水补给","季节性积雪融水补给","湖泊与沼泽水补给","潮汐补给"],"I15":["3"]},{"I1":"bab0ed63-6856-4e9b-aab5-4a38b2846ed3","I2":["（ ）是自然地理系统的基本组成部分。"],"I3":1,"I6":["大气","岩石地形复合体","水分","有机界"],"I15":["1"]},{"I1":"0a020f67-1a3b-4a41-94b5-dd2a7193f75d","I2":["潮汐的变化规律最为显著的是（ ）。"],"I3":1,"I6":["多年变化","年华化","日变化","季变化"],"I15":["2"]},{"I1":"358c2867-a24a-4534-ac15-3ac3a155947a","I2":["下列现象中由公转产生的是（ ）。"],"I3":1,"I6":["昼夜","日月星辰的东升西落","昼夜长短变化","昼夜交替"],"I15":["2"]},{"I1":"70db390a-d809-4299-99ae-0044772c17c6","I2":["右图景观<img src="http://file.open.com.cn/ueditorupload/image/2020/02/07/6371663253046845389872162.png" title="微信图片_20200207003510.png" alt="微信图片_20200207003510.png">体现出了的地球圈层包括（   ）。<br><br>"],"I3":1,"I6":["水圈、生物圈<br><br>","水圈、岩石圈、生物圈<br><br>","水圈、岩石圈、大气圈<br><br>","水圈、岩石圈、生物圈、大气圈<br><br>"],"I15":["3"]},{"I1":"dde1b538-e383-4bc8-8232-74b19fb710ba","I2":["地球上产生昼夜更替的主要原因是( )。"],"I3":1,"I6":["地球是一个不透明、不发光的椭球体","地球绕太阳的运动","地球自转","地轴同赤道面成23.5夹角"],"I15":["2"]},{"I1":"000ae417-e406-4368-ae63-9c8eba3b3d44","I2":["下列关于地下水说法不正确的是（ ）。"],"I3":1,"I6":["上层滞水主要接受大气降水或地表水下渗进行补给","潜水一般埋藏较深，难以开发利用","气候、地表水的变化对承压水的影响较小","当承压水位高于地面高程时，承压水又可称为自流水"],"I15":["1"]},{"I1":"92d00bb3-ff98-4d83-9a43-495981ac5d7c","I2":["硬度为10的矿物是（ ）。"],"I3":1,"I6":["石英","石膏","金刚石","滑石"],"I15":["2"]},{"I1":"1e3031e5-c454-4e66-adec-e8766f39cc0a","I2":["四幅地质构造图中，有地堑、向斜山景观的分别是（ ）。"],"I3":1,"I6":["①②","②③","③④","①④"],"I15":["1"]},{"I1":"188c7e74-5d05-4d2c-aae3-624306078ef0","I2":["离地球最近的恒星是（ ）。"],"I3":1,"I6":["北极星","天狼星","太阳","比邻星"],"I15":["2"]},{"I1":"459f83b9-7599-4824-9807-a1c379f802a6","I2":["下列不属于土壤化学性质的是（ ）。"],"I3":1,"I6":["阳离子交换量","酸碱性","孔隙度","缓冲性"],"I15":["2"]},{"I1":"029fced9-3caa-47ee-96a4-d93a518994d1","I2":["下列那种因素属于影响水循环的气象因素（ ）。"],"I3":1,"I6":["地貌","植被","气温","土壤"],"I15":["2"]},{"I1":"47ac9e5d-4209-450a-bfca-2510fd54eff4","I2":["完整的垂直带谱其顶带应该是：（ ）。"],"I3":1,"I6":["永久冰雪带","基带","树线","高山草甸带"],"I15":["0"]},{"I1":"98c499ae-3d49-4788-aa1e-11269e39a711","I2":["土壤是植物生长发育的基质，土壤对于植物的影响决定于它的（ ）。"],"I3":1,"I6":["物理特性、化学特性和生物学特性","水分、肥力和空气","水分、温度、空气和肥力","机械组成、物理性质、土壤缓冲性"],"I15":["0"]},{"I1":"7d13dc0e-35ca-4794-b697-c1奥鹏四川农业大学在线考核满分答案参考fcc20dd854","I2":["地球表层的能量基础是（ ）。"],"I3":1,"I6":["太阳能","生物能","水能","风能"],"I15":["0"]},{"I1":"d33c652c-6245-4d72-ba66-26d580ef2cf7","I2":["雨热同季是（ ）的特征。"],"I3":1,"I6":["地中海气候","干湿季气候","季风气候","大陆性气候"],"I15":["2"]},{"I1":"e4add5f2-43fc-4785-9791-f66b4e0b42e2","I2":["在下列褶皱中，褶皱强度最大的是（ ）。"],"I3":1,"I6":["直立褶皱","倒转褶皱","翻卷褶皱","倾斜褶皱"],"I15":["2"]},{"I1":"7491dfa3-b779-4c3b-8d97-ca374840ea0c","I2":["土壤是个多相分散体系，由（ ）等不同物质组成。"],"I3":2,"I6":["有机质","矿物质","空气","水分"],"I15":["0","1","2","3"]},{"I1":"a90cc6fa-bff5-49ed-a4f0-4eb26f3abfbb","I2":["关于土壤颜色下列哪些观点是正确的（ ）。"],"I3":2,"I6":["许多土类是用颜色来命名的","土壤黑色一般与腐殖质的含量有关","目前世界通用的土壤颜色系列是用色调、亮度和彩度来表示的","土壤白色主要与三氧化物的含量有关"],"I15":["0","1","2"]},{"I1":"1e577675-611f-45c4-9023-13a6e475756d","I2":["阶地按组成物质及其结构的差异分为（ ）。"],"I3":2,"I6":["侵蚀阶地","堆积阶地","基座阶地","高级阶地"],"I15":["0","1","2"]},{"I1":"4a9877fc-f67d-4b02-b197-ef640edceff7","I2":["大陆纬度地带性包括（ ）。"],"I3":2,"I6":["气候纬度地带性","植被纬度地带性","土壤纬度地带性","动物界的纬度地带性"],"I15":["0","1","2","3"]},{"I1":"60885502-ad2c-4a98-9452-116e52ad30e4","I2":["下列哪些说法是正确的（ ）。"],"I3":2,"I6":["土壤总是处于大气圈、水圈、岩石圈、生物圈的界面上","土壤是自然条件共同作用的产物","土壤有支持和调节生物过程的功能","土壤对岩石具有一定的保护作用"],"I15":["1","2","3"]},{"I1":"13491c22-bdc1-4770-aec4-9bc85368c76a","I2":["大气环流包括（ ）"],"I3":2,"I6":["全球环流","季风环流","局地环流","西风漂流"],"I15":["0","1","2"]},{"I1":"6356251d-32f5-44f9-a5aa-f304bbef48dd","I2":["地球外圈（或大气圈）由（ ）和对流层五部分组成。"],"I3":2,"I6":["散逸层（或扩散层）","电离层（暖层）","中间层（高空对流层）","平流层"],"I15":["0","1","2","3"]},{"I1":"3b517ffc-8da1-470f-b94c-d110bf32aa3d","I2":["河流的地表水的补给方式有（ ）。"],"I3":2,"I6":["雨水补给","季节性积雪融水及冰雪融水补给","湖泊与沼泽水补给","深层地下水补给"],"I15":["0","1","2"]},{"I1":"f6e9cbe1-053b-494c-bdcd-cff17a0a5dd2","I2":["水系形状各种各样，归纳起来有（ ）。"],"I3":2,"I6":["扇状","羽状","树枝状","平行状","格子状"],"I15":["0","1","2","3","4"]},{"I1":"2fdf56c7-8719-436c-909d-07109a7975ec","I2":["地方性分异规律的表现格局大致有（ ）。"],"I3":2,"I6":["系列性","组合性","镶嵌性","微域性"],"I15":["0","1","2"]},{"I1":"f52f5299-6cb5-4fd1-9c1c-70012298d98b","I2":["土壤的水平分布规律包括土壤纬度地带性规律和经度地带性规律。（ ）"],"I3":3,"I6":["对","错"],"I15":["0"]},{"I1":"6621844d-a4cd-497e-b897-4602d04e7112","I2":["岩溶地貌主要是分布最广的硫酸盐经溶蚀作用形成的地面坎坷嶙峋、地下洞穴发育的特殊地貌。（ ）"],"I3":3,"I6":["对","错"],"I15":["1"]},{"I1":"2fee7e5e-3f5e-455c-8bcf-e8289cd39f65","I2":["正午太阳高度角随纬度的增加而减小，因此气温的日较差也随纬度的增加而减小。（ ）"],"I3":3,"I6":["对","错"],"I15":["0"]},{"I1":"9b8b8bdb-c8d3-4269-af32-060e1c130132","I2":["水圈是在地球演化过程中形成的一个特殊圈层。（ ）"],"I3":3,"I6":["对","错"],"I15":["1"]},{"I1":"a54f37a2-f696-4a4a-97e0-b01955964049","I2":["正地形是指高度高于海平面的地形。（ ）"],"I3":3,"I6":["对","错"],"I15":["1"]},{"I1":"693fbb13-7a24-4dd7-968a-709b1b0238d3","I2":["土壤形成过程，实质上是物质的地质大循环和营养元素的生物小循环矛盾与统一的结果。（ ）"],"I3":3,"I6":["对","错"],"I15":["0"]},{"I1":"3c4125bf-bbfe-4f48-9f2d-cb6ceea5ad26","I2":["地球内能是非地带性地域分异的能量基础。（ ）"],"I3":3,"I6":["对","错"],"I15":["0"]},{"I1":"5b154419-c8ef-4f11-af0a-71d569167218","I2":["大兴安岭西麓的低山丘陵以及东北平原的黑土、黑钙土区的主要植被类型为寒温带针叶林。（ ）"],"I3":3,"I6":["对","错"],"I15":["1"]},{"I1":"51e075d3-86c1-4640-b11b-0dd9606ed56f","I2":["根据锋两侧冷、暖气团的移动方向和结构状况，可将锋分为三种类型。（ ）"],"I3":3,"I6":["对","错"],"I15":["0"]},{"I1":"b7bd27e1-f5c1-4039-9900-bc74631ed319","I2":["地球是一个完美的球体。（ ）"],"I3":3,"I6":["对","错"],"I15":["1"]},{"I1":"a6336bc3-b1bb-44a0-832b-456b85eb5b90","I2":["简述岩石循环及过程。"],"I3":6,"I6":["满分答案问询微信：424329