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1.Analysing on Moisture Index, Water Economization and Adversity Resistance of Optimum Irrigation for Winter Wheat in North china
华北地区冬小麦优化灌溉的水分指标与节水性、抗逆性分析收藏指正
2.The species richness of herb layer was fitted in the topographic and soil feature factors, as well as the topographic relative moisture index (TRMI) by the generalized linear models (GLM).
通过广义线性模型(generalizedlinearmodels,GLM)拟合了草本层物种丰富度与地形因子、土壤因子以及地形相对湿度指数(TRMI)之间的关系。收藏指正
3.In this area,there are 6 and 7 remarkable moist and dry periods,respectively. The reconstructed moisture index from March to June in the recent 200 years has stable periods of 11,16,5,8,3 and 32 a.
天山东段近200 a来3~6月湿润指数序列的显著周期是11 a,然后依次存在16 a、5 a、8 a、3 a和32 a的稳定周期.收藏指正
4.Thornthwaite′s method on calculating PE and climatic classificationhas been applied on computing data from 671 climatological observationstations in China. A geographic regression model of potential evapotran-spiration is resulted as APE=2037. 98-18. 8308LAT-4.5801 LONG-0.157861ALT. The resulted APE and moisture index, Im are closely cor-related with the major vegetation types and their distribution pattern inChina.
Thorn thwaite计算PE与气候分类方法对我国671个气候台站资料计算分析结果,得出可能蒸散的地理回归模型为: APE=2037.98-18.8308LAT(纬度)-4.5801LONG(经度)-0.157861ALT(海拔) APE与湿度指数Im与我国植被的主要类型及其分布格局有密切相关性。收藏指正
5.The optimum soil moisture content index about tomato seedling bed irrigation was conducted out in early spring .
对番茄早春育苗的苗床灌溉最佳土壤含水量上限数值进行了试验研究。收藏指正
6.The Study on germination characteristics of Lagerstroemia indica CV.Petite Pinkie seeds was carried out,which might be affected by four factors including temperature,lighting period,soil moisture and the value of pH. The conclusion showed that they could germinate under the wider content of soil moisture while the Index of seed vigour were the highest from 40% to 60% than other moisture conditions.
就温度、光照、土壤水分及pH值对矮生紫薇种子萌发的影响进行了研究,结果表明:种子萌发的土壤水分条件较宽,但40%~60%时的活力指数高;收藏指正
7.According to the concept of soil-moisture-balance in Palmer-drought-model,daily drought index(DDI) is defined by available water content(AWC) below level soil. AWC was simulated day by day using daily data of temperature and rainfall.
参考帕默尔(Palm er)旱度模式中土壤水分平衡概念,提出以逐日气温和降水资料,逐日滚动模拟土壤有效水分,并以下层土壤有效含水量构建干旱强度动态指数(DD I).收藏指正
8.For bare land or low vegetation coverage conditions(NDVI≤0.3),apparent thermal inertia(ATI) based on the thermal inertia theory can be used to deduce the soil moisture and for high vegetation coverage,vegetation-soil-water index(VSWI) method.
裸地或低植被覆盖条件(NDVI≤0.3)采用基于热惯量理论的表现热惯量法(ATI)、高植被覆盖条件(NDVI>0.3)采用作物供水指数法(VSW I)来反演土壤含水量。收藏指正
9.?Based on the experimental data of evapotranspiration in the field, considering the meteorological conditions, cotton biological properties and soil moisture state, a calculation model for actual evapotranspiration of cotton field is developed by means of the Priestley?Taylor model, cotton leaf area index and relative effective soil moisture. The routine meteorological and agrometeorological data would be only needed to calculate the evapotranspiration by using the model, and there is a good precision. It can be used in arid area in China easily.
在农田蒸散试验资料的基础上,综合考虑影响棉田实际蒸散的气象条件,棉花生物学特性和土壤水分等因素,利用Priestley-Taylor模式、棉花叶面积指数和相对有效土壤湿度建立了棉田实际蒸散量的计算模式.该模式仅需常规气象和农业气象资料,具有较高的精度,便于在干旱区推广使用.收藏指正
10.Polarization index PI of the SSM/I microwave radiance is derived from the radiative transfer equation, and is applied to identifying spatial and temporal variations of the terrain surface moisture.
由辐射传输方程推导星载被动微波遥感SSMI辐射观测的极化指数PI,凸现地表土壤湿度的变化与距平异常ΔnPI,用特征性指数PI、ΔnPI和散射指数SI来监测大尺度陆地地面的降雨和地区土壤湿度、洪涝汛情的变化.收藏指正
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