Results 41 to 50 of about 965 (197)
, 2019 以典型的中度退化天坑——巴家陷塘天坑为例,对其倒石坡生态交错带森林群落优势种种群进行生态位特征分析,以期为喀斯特天坑的生物多样性保护及天坑地表区域植被的生态修复提供科学参考.结果表明:土壤养分铵态氮、速效钾、有效磷相较于土壤水分和温度对天坑物种分布影响最显著,解释量分别为37.4%、32.8%、29.3%.随着天坑倒石坡坡位(坑口-上坡位-中坡位-下坡位-坑底)的变化,其林下植物生活型由常绿旱生向常绿湿中生变化,草本种群生态位重叠程度较灌木种群更大.灌木植物密花荚蒾、小雀花和草本植物一把伞南星 ...
冯洁 +7 more
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Shuitu Baochi Xuebao, 2022 为了解内蒙古河套灌区农田防护林内冻融期土壤水盐状况及运移规律, 在2020年10月至2021年4月实测土壤水分、盐分、温度及相关气象数据, 并进行相关分析。结果表明: 土体表层温度波动较大, 随土层深度加深土体温度变化逐渐平缓。冻结期气温下降速率低于消融期气温回升速率, 加之土壤温度变化的滞后性, 冻结期比消融期长10天左右。季节性冻融冻结作用导致表层土壤含水量升高、深层含水量降低, 消融解冻时期, 土壤含水量逐渐降低。两侧林带农田边缘(0.3 H、4 H)土壤表层含水量相比农田内部(1 H、2 H、3
郝可心 +4 more
doaj
Contribution of Different Processes in Wetland Soil N_2O Production in Different Restoration Phases of the Yellow River Estuary, China [PDF]
, 2014 采用时空替代法,选择黄河口生态恢复前后未恢复区(R_0)、2007年恢复区(R_(2007))和2002年恢复区(R_(2002))的芦苇湿地为研究对象,分析了生态恢复工程对湿地土壤N_2O产生不同过程与贡献的影响. 结果表明,尽管不同恢复阶段湿地土壤N_2O总产生量差异明显,但总体均表现为N_2O释放. 恢复区湿地土壤的N_2O产生量大于未恢复区.
孙万龙 +4 more
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Developments and applications of terrestrial biosphere model [PDF]
, 2020 Exchanges of energy and matter between terrestrial biosphere and atmosphere and hydrosphere create critical feedbacks to Earth’s climates. To quantify how terrestrial ecosystems respond and feedback to global changes, terrestrial biosphere model (TBM ...
Chang, J., Peng, S.-S., Yue, C.
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Shuitu Baochi Xuebao, 2017 为研究煤矿区用矸石作为垫底基质进行土壤剖面重构土壤水分再分布过程和剖面热扩散与气体浓度变化特征，以指导工程设计和重构土壤熟化技术应用，在实验室设计了一种煤矿区重构土壤水气热运移模拟装置，通过布设在土柱系统不同深度的温湿度传感器和CO2浓度检测仪，连续监测重构土壤剖面含水量、温度和CO2浓度。结果表明：煤矸石层具有良好的阻水性，阻碍水分的入渗，增加上层土壤的持水能力。但是，煤矸石的持水性差，煤矸石层的含水量远低于土壤层10%左右；煤矸石具有更佳的热扩散性，在加热过程中煤矸石层的温度远大于土壤层 ...
王, 陈清华
doaj
Characteristics and Influencing Factors of Soil CH4 and N2O Fluxes in Typical Broad-leaved Forests in the Yangtze River Delta Region, China [PDF]
[Objective] The forest coverage rate in the Yangtze River Delta region reaches 33.4%, and the underlying surface soil may have an important impact on the regional greenhouse gas budget.
CHEN Bingjiang +7 more
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Shuitu Baochi Xuebao, 2022 为探究在非灌溉季节施加生物炭对滴灌棉田耕层土壤水热特性和三相结构的调控效应。设置生物炭15(B1),30(B2),45(B3),60(B4),0(B0) t/hm25个施加量,分析其对新疆滴灌棉田非灌溉季节耕层土壤(0—40 cm)三相结构、总孔隙度、土壤温度和土壤含水率的影响。结果表明:与对照处理相比,施炭处理使土壤固相体积降低2.58%~10.74%,总孔隙度增加3.38%~12.05%;同时,施炭处理的融后土壤质量含水率较对照处理提高1.07%~2.65%;施炭处理的土壤导热系数降低 ...
邹瑞晗 +4 more
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环境因子和生物因子对黄河三角洲滨海湿地土壤呼吸的影响 [PDF]
, 2016 Using the Li-8150 multichannel automatic soil CO2efflux system, soil respiration was measured continuously over a one-year period in a coastal wetland in the Yellow River Delta, China.
Chen, Liang +6 more
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Structure and Control Optimization of the Buried Pipe Group Heat Exchanger With Vertical Inlet and Flat Outlet [PDF]
ObjectivesIn order to improve the utilization efficiency of shallow geothermal energy, it is urgent to optimize the structure and control of ground heat exchanger, which affects the performance of ground source heat pump system.MethodsA model of the ...
MA Peifa +3 more
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Shuitu Baochi Xuebao, 1995 研究了黄土丘陵区油松人工林内降不、相对温度、土壤水分、气温；地温等水热因子的变化规律，结果表明：林冠和枯枝叶层对降水截留作用强，林地仅获得７０％的林外降水量；月平均相对温度林内均低于林外，年平均相对湿度林内较林外低６．０％；林地土壤水分环境不良，水分恢复能力也较；林分对各月气温影响程度不同，年平均气温林内高于林外；林内土壤温度及其较差均低于林外，枯枝落叶层对土壤温度影响明显。
陈云明 吴钦孝
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