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地下水灌溉回水对黄河流域化学风化CO_2消耗估算的影响 被引量:2
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作者 王健 王亮 张龙军 《中国海洋大学学报(自然科学版)》 CAS CSCD 北大核心 2014年第9期89-97,共9页
本文根据2012年6月和2013年5月采集的河南、宁夏和内蒙等引黄灌区地下水实测数据,并结合文献数据,探讨了引黄灌区地下水离子组成的分布特征。结果表明:因受蒸发作用和人为因素影响较小,深层地下水矿化度和HCO-3的浓度小于浅层水,但HCO-... 本文根据2012年6月和2013年5月采集的河南、宁夏和内蒙等引黄灌区地下水实测数据,并结合文献数据,探讨了引黄灌区地下水离子组成的分布特征。结果表明:因受蒸发作用和人为因素影响较小,深层地下水矿化度和HCO-3的浓度小于浅层水,但HCO-3占阴离子比例大于浅层水。因各灌区蒸发量、降雨量以及岩性的不同,浅层地下水化学组成和风化来源阳离子浓度在各灌区表现出较大的差异。HCO-3占阴离子的比例在河南灌区最高,内蒙灌区中部和宁夏灌区次之,内蒙灌区东西部最低。河南和内蒙灌区风化来源阳离子浓度相差不多,均大于宁夏灌区。灌区浅层地下水灌溉回水高估的黄河流域化学风化消耗CO2的量为23.3×108 mol/a。 展开更多
关键词 引黄灌区 地下水灌溉回水 化学风化 CO2消耗量
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水稻节水增温灌溉技术 被引量:2
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作者 吴运玲 《黑龙江农业》 2003年第3期45-45,共1页
关键词 水稻 节水增温灌溉 水层管理 叠水板 回水灌溉 宽浅式灌水渠
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井水种稻提高水温的几项技术措施
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作者 赵丽英 朱化安 《农村科学实验》 2005年第8期8-8,共1页
在寒地稻作区,井水种稻面积较大,由于气温低,井水凉,对水稻提高产量不利,尤其是在高寒地区,山尖冷凉地区、大面积利用井水种稻,其影响水稻产量和成熟更为不利。因此采取有效措施,提高井水种稻的水温对促进发展水稻生产有着重要... 在寒地稻作区,井水种稻面积较大,由于气温低,井水凉,对水稻提高产量不利,尤其是在高寒地区,山尖冷凉地区、大面积利用井水种稻,其影响水稻产量和成熟更为不利。因此采取有效措施,提高井水种稻的水温对促进发展水稻生产有着重要意义。 展开更多
关键词 水稻 井水 水温 晒水池 塑料薄膜 回水灌溉
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Analysis of Factors Determining the Demand for Water: A Case Study of Sabie Administrative Post, Moamba District, Mozambique
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作者 Helder Antonio Manjate Joao Enganado Mutondo 《Journal of Agricultural Science and Technology(B)》 2016年第1期18-26,共9页
Water is an important resource for human being. However, it has been increasingly becoming the limited resource. Therefore, the debate of water issues has been centered in mechanisms to implement sustainable water man... Water is an important resource for human being. However, it has been increasingly becoming the limited resource. Therefore, the debate of water issues has been centered in mechanisms to implement sustainable water management. Hence, understanding the determinants of water demand might help design appropriate water management policies, however, they are not known in Mozambique. Due to the lack of knowledge about the determinants of water demand in Mozambique in general and in Sabi6 in particular, the present study was conducted to analyse the factors determining the water demand for irrigation and domestic use using a linear regression model and travel cost method, respectively. The results show that an increase in 1 h of irrigation time increases the quantity demanded of irrigation water by 362.04 m3 and an increase in one irrigation per week increases the quantity demanded of irrigation water by 1,065.61 m3. Additionally, the results show that an increase in 1% of time spent in water collection decreases the number of trips by 0.3% and an increase in 1% in the number of household members involved in water collection decreases the number of the water collection trips by 0.23%. Household having private taps have less number of trips collecting water compared to those collecting water from public taps and boreholes as well as rivers. Therefore, the water demand for irrigation is determined by time spent for irrigation per day and the number of irrigations per week, and water demand for domestic use is determined by time spent for water collection, number of household members involved in water collection, the volumes of the containers used to collect water, the number of containers used to collect water, the quantity of water consumed by the household as well as the main source of water (river, boreholes and public tap). 展开更多
关键词 Domestic use irrigation use water demand.
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