By Sarah H. Jacoby
Love and Liberation reads the autobiographical and biographical writings of 1 of the few Tibetan Buddhist girls to checklist the tale of her existence. Sera Khandro Künzang Dekyong Chönyi Wangmo (also known as Dewé Dorjé, 1892-1940) was once remarkable not just for reaching spiritual mastery as a Tibetan Buddhist visionary and guru to many lamas, monastics, and laity within the Golok sector of jap Tibet, but additionally for her candor. This booklet listens to Sera Khandro's conversations with land deities, dakinis, bodhisattvas, lamas, and fellow non secular neighborhood individuals whose voices interweave together with her personal to relate what's a narrative of either love among Sera Khandro and her guru, Drimé Özer, and religious liberation.
Sarah H. Jacoby's research specializes in the prestige of the feminine physique in Sera Khandro's texts, the advantage of celibacy as opposed to the expediency of sexuality for spiritual reasons, and the adaptation among profane lust and sacred love among female and male tantric companions. Her findings upload new dimensions to our realizing of Tibetan Buddhist consort practices, complicating typical scriptural displays of male topic and feminine aide. Sera Khandro depicts herself and Drimé Özer as inseparable embodiments of perception and strategy that jointly shape the Vajrayana Buddhist imaginative and prescient of entire buddhahood. by way of advancing this complementary sacred partnership, Sera Khandro carved a spot for herself as a feminine virtuoso within the male-dominated sphere of early twentieth-century Tibetan faith.
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Influent water is sampled via a well prior to contact with limestone. Four sampling wells are spaced evenly along the length of the drain. Howe Bridge 2. Discharge from another abandoned well is treated in an S-shaped limestone drain. Influent water is sampled via a well as the water flows into the limestone drain. Two sampling wells are along the length of the drain. Elklick. 9 m) of crushed, low-pyrite sandstone at the head of the limestone drain. Influent water is sampled at a well in this sandstone.
Untreated inflow was intercepted within the trench or was piped into the drain. If possible, trenches were excavated in clay or liners were installed to prevent leakage. Generally, the outflow pipe from each of the flooded drains was extended to a level above the top of the limestone to ensure continuous inundation of the limestone and to minimize airflow into the drains. Additional information is provided here and in Table I. Howe Bridge 1. Discharge from an abandoned well is captured and piped to the limestone drain.
Environ. Engin. Div. EE3A25^H\. Robertson, W. D. and Cherry, J. A. (1995). In situ denitrification of septic-system nitrate using reactive porous media barriers: Field trials. Ground Water 33, 99-111. Rumar, R. , and Mitchell, J. K. ) (1995). S. Department of Energy. Available from National Technical Information Service, No. PB96-180583, 437. Scott, M. , Metting, F. , Fruchter, J. , and Wildung, R. E. (1998). Research investment pays off. Soil Groundwater Cleanup October 6-13. Spangler, R. , and Morrison, S.