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Water quality parameter as a predictor of small watershed land cover

机译:水质参数可预测小流域土地覆盖

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Different land cover affect water quality through interaction at root microsite during various phase of nutrient uptake. Litter layer and its decomposition, microbial interactions and physico-mechanical role to soil and water by vegetation influence directly or indirectly the draining water quality. However, the role of vegetation on water is dependent on scale of space and time. Water samples from creek and seepage were collected from mountainous catchment of varied land cover in southeastern Bangladesh to comprehend land cover effect in small catchment using paired watershed method. From the water sample analysis for common anions and cations, we revealed that water sample of shifting cultivated catchment contains higher SO42- and NO3- and lower HCO3-, Na+, K+ and TDS compared to natural vegetation area. The cations of water sample showed a regular trend than anions with land cover change in different sampling sites. Difference between creek and seepage water chemistry attributed to soil-water interaction during digging process associated to the shifting cultivation, plantation and agricultural landuse. Shifting cultivation and agriculture catchments exhibit higher NO3-N, SO42- total-phosphorous as well as base cations (Ca2+, Mg2+ and Na+) concentrations. From this study it revealed that anions such as SO42-, NO3-, Na+ and TDS are can be consistently use as an indicator water quality parameter to discern land cover change in this mountainous watershed. Monitoring of sensitive parameter would be effective to understand land cover change dynamics in a watershed. It was also sufficiently proved that the leaching of this ions in waterbodies from a landuse causing enrichment of the repository water body, where chemical fertilization is not seen being practiced for agriculture and forestry during the whole field campaign. The impacts of shifting cultivation and agricultural land uses on creek and seepage water chemistry are unlikely to lead to damaging consequences for the aquatic biota at present and in the near future in its current states and extends.
机译:在养分吸收的各个阶段,不同的土地覆盖通过根部微观站点的相互作用影响水质。枯草层及其分解,微生物相互作用和植被对土壤和水的物理力学作用直接或间接影响排水水质。但是,植被在水上的作用取决于空间和时间的规模。从孟加拉国东南部多处土地覆盖的山区流域收集了小溪和渗流的水样,以成对流域方法了解了小流域的土地覆盖效应。通过对常见阴离子和阳离子的水样分析,我们发现与自然植被面积相比,流域耕地流域的水样中SO42-和NO3-含量较高,而HCO3-,Na +,K +和TDS含量较低。在不同的采样地点,水样中的阳离子与土地覆盖变化的阴离子相比呈现出规律的趋势。小溪和渗流水化学之间的差异归因于挖掘过程中土壤与水的相互作用,这与耕种,种植和农业土地利用的转移有关。轮换种植和农业流​​域的NO3-N,SO42-总磷以及碱性阳离子(Ca2 +,Mg2 +和Na +)浓度较高。从这项研究中可以看出,诸如SO42-,NO3-,Na +和TDS之类的阴离子可以始终用作指示水质参数,以识别该山区流域的土地覆盖变化。监测敏感参数将有效了解流域的土地覆盖变化动态。也已经充分证明,这种离子从土地利用中浸出到水体中会导致储存水体的富集,在整个田间运动中,农业和林业并未进行化学施肥。耕作和农业用地转移对小河和渗流水化学的影响不太可能对目前和不久的将来在其当前状态和范围内对水生生物群造成破坏性后果。

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