陕西省土壤温度和水分状况估算
发布时间：2019-02-13 14:17
【摘要】：土壤温度和水分状况是中国土壤系统分类的两个重要诊断特性。土壤的水热状况受近地表温度和降水的直接影响,可以通过气候因素来估算土壤水分和温度状况。以陕西省85个气象台站连续30年的地面气象数据为基础,采用地统计与纽荷模型(JNSM)相结合的方法研究了陕西省土壤温度和水分状况及其空间分布。结果表明,土壤温度状况表现为:秦岭山区及其以北为温性,汉江河谷地区及其以南为热性;土壤水分状况表现为:长城以北为干旱,陕北黄土高原地区和关中盆地为半干润,秦岭以南为湿润,常湿润仅在最南端镇巴县和镇坪县的小部分南部地区存在。
[Abstract]:Soil temperature and soil moisture are two important diagnostic characteristics of soil classification in China. The water and heat status of soil is directly affected by near-surface temperature and precipitation, and the soil moisture and temperature can be estimated by climatic factors. Based on the surface meteorological data of 85 meteorological stations in Shaanxi Province for 30 consecutive years, the soil temperature and moisture status and their spatial distribution in Shaanxi Province were studied by means of geostatistics and (JNSM) model. The results show that the soil temperature is: Qinling mountain area and its north is warm, Hanjiang River valley area and its south is thermal; The soil moisture conditions are as follows: drought in the north of the Great Wall, semi-dry and moist in the Loess Plateau and Guanzhong Basin in northern Shaanxi, and humid in the south of Qinling Mountains, usually only in the southern part of Zhenba County and Zhenping County in the southernmost part.
【作者单位】： 西北农林科技大学资源环境学院;
【基金】：国家科技基础性工作专项项目(2014FY110200A08)资助
【分类号】：S152
[Abstract]:Soil temperature and soil moisture are two important diagnostic characteristics of soil classification in China. The water and heat status of soil is directly affected by near-surface temperature and precipitation, and the soil moisture and temperature can be estimated by climatic factors. Based on the surface meteorological data of 85 meteorological stations in Shaanxi Province for 30 consecutive years, the soil temperature and moisture status and their spatial distribution in Shaanxi Province were studied by means of geostatistics and (JNSM) model. The results show that the soil temperature is: Qinling mountain area and its north is warm, Hanjiang River valley area and its south is thermal; The soil moisture conditions are as follows: drought in the north of the Great Wall, semi-dry and moist in the Loess Plateau and Guanzhong Basin in northern Shaanxi, and humid in the south of Qinling Mountains, usually only in the southern part of Zhenba County and Zhenping County in the southernmost part.
【作者单位】： 西北农林科技大学资源环境学院;
【基金】：国家科技基础性工作专项项目(2014FY110200A08)资助
【分类号】：S152
【相似文献】
相关期刊论文 前10条
1 赵景波;郁科科;邵天杰;张冲;罗万银;张正Pr;董治宝;;腾格里沙漠沙层水分状况初步研究[J];资源科学;2011年02期
2 邓波儿,冯跃华,陈明亮;水分状况对菜地土壤氮素转化运移的影响[J];湖北农业科学;1993年11期
3 陈杰,龚子同,阮心玲,Blume HP;南极半岛海洋气候区的土壤——Ⅲ.冻-融作用与水分状况[J];土壤;2004年01期
4 李道真;冻结期冻土层水分状况的研究[J];土壤通报;1966年01期
5 高国治;景元书;张斌;王明珠;;低丘红壤坡耕地的水分状况变化及其调控[J];土壤;2005年06期
6 曾宪竟，徐祝龄，杨培龄，，徐驰;黄河古道细质沙土水分性状的研究[J];中国农村水利水电;1996年04期
7 乔樵,沈善敏,曾昭顺;东北北部黑土水分状况之研究——Ⅱ.黑土农业水分状况及水分循环[J];土壤学报;1979年04期
8 熊运章;;γ射线法则定土柱内水分移动之初步试验[J];西北农林科技大学学报(自然科学版);1960年02期
9 李玉山;(土娄)土水分状况与作物生长[J];土壤学报;1962年03期
10 霍明德;陈行军;;陇东西南部黄土高原沟壑区水分状况与造林关系的分析[J];甘肃林业科技;1984年02期
相关会议论文 前2条
1 吉海彦;马m
本文编号：2421634
本文链接：https://www.wllwen.com/kejilunwen/nykj/2421634.html
